{"id":7868,"date":"2023-08-16T05:18:27","date_gmt":"2023-08-16T05:18:27","guid":{"rendered":"https:\/\/goliatminerals.wpenginepowered.com\/?page_id=7868"},"modified":"2026-10-23T15:11:31","modified_gmt":"2026-10-23T15:11:31","slug":"societe-marocaine-specialisee-dans-lexploration-et-le-developpement-de-projets-miniers","status":"publish","type":"page","link":"https:\/\/www.goliatminerals.com\/fr\/societe-marocaine-specialisee-dans-lexploration-et-le-developpement-de-projets-miniers\/","title":{"rendered":"Potfolio Goliath"},"content":{"rendered":"<div class=\"wpb-content-wrapper\"><section data-row-bg=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/09\/Mesa-de-trabajo-1-copia-3.jpg?id=9241\" data-slideshow-bg=\"true\" data-slideshow-options='{\"imageArray\":[{\"src\":\"https:\\\/\\\/www.goliatminerals.com\\\/wp-content\\\/uploads\\\/2025\\\/10\\\/PHOTO-2025-10-22-17-31-44-3.jpg\",\"alt\":\"Row Background 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Background Image\"},{\"src\":\"https:\\\/\\\/www.goliatminerals.com\\\/wp-content\\\/uploads\\\/2025\\\/10\\\/DSCN0482.jpg\",\"alt\":\"Row Background Image\"}]}' data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1761556975075 liquid-row-shadowbox-6aea90e7c0944 vc_row-has-fill vc_row-has-bg vc_row-o-full-height vc_row-o-columns-middle vc_row-o-equal-height vc_row-o-content-middle vc_row-flex\"><span class=\"row-bg-loader\"><\/span><div class=\"liquid-row-overlay\" style=\"background:rgba(46, 46, 46, 0.45)\"><\/div><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 vc_col-md-6 liquid-column-6aea90e7c1339\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  data-custom-animations=\"true\" 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data-custom-animations=\"true\" data-ca-options='{\"triggerHandler\":\"inview\",\"animationTarget\":\".lqd-lines .split-inner\",\"duration\":700,\"delay\":100,\"easing\":\"easeOutQuint\",\"direction\":\"forward\",\"initValues\":{\"scale\":1},\"animations\":{\"scale\":1}}' data-split-options='{\"type\":\"lines\"}' data-text-rotator=\"true\"><span class=\"ld-fh-txt\"> Eficiencia y Excelencia en cada Etapa del Proceso<\/span><\/h2><\/div><style>.ld_spacer_6aea90e7c2119{height:25px;}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e7c2119\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-12 vc_col-md-6 text-left text-md-center liquid-column-6aea90e7c2277\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  data-custom-animations=\"true\" 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class=\"lqd-frickin-img-inner\">\n\n\t\t<span class=\"lqd-frickin-img-bg\"><\/span><!-- \/.lqd-frickin-img-bg -->\n\t\t<div class=\"lqd-frickin-img-holder\"><figure data-responsive-bg=\"true\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion8.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion8.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion8-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion8-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure><\/div>\n\t<\/div><!-- \/.lqd-frickin-img-inner -->\n<\/div><!-- \/.lqd-frickin-img --><style>.ld_spacer_6aea90e7de8ea{height:50px;}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e7de8ea\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-12 vc_col-md-offset-1 vc_col-md-5 liquid-column-6aea90e7deaf7\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90e7dec92\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90e7dedf8\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  data-custom-animations=\"true\" data-ca-options='{\"triggerHandler\":\"inview\",\"animationTarget\":\"all-childs\",\"duration\":\"1200\",\"startDelay\":\"400\",\"delay\":\"150\",\"easing\":\"easeOutQuint\",\"direction\":\"forward\",\"initValues\":{\"translateX\":-44,\"opacity\":0},\"animations\":{\"translateX\":0,\"opacity\":1}}'><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90e7deec6 h2{font-size:50px;line-height:1.15em;font-weight:600;}.ld_fancy_heading_6aea90e7deec6 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e7deec6\">\n\t<h2 class=\"lqd-highlight-underline lqd-highlight-grow-left\" data-fittext=\"true\" data-fittext-options='{\"compressor\":0.5,\"maxFontSize\":\"50\",\"minFontSize\":\"32\"}' data-split-text=\"true\" data-custom-animations=\"true\" data-ca-options='{\"triggerHandler\":\"inview\",\"animationTarget\":\".lqd-lines .split-inner\",\"duration\":700,\"delay\":100,\"easing\":\"easeOutQuint\",\"direction\":\"forward\",\"initValues\":{\"scale\":1},\"animations\":{\"scale\":1}}' data-split-options='{\"type\":\"lines\"}'><span class=\"ld-fh-txt\"> Innovaci\u00f3n para el Futuro Minero<\/span><\/h2><\/div><style>.ld_fancy_heading_6aea90e7df2f2 p{font-size:20px;line-height:1.7em;color:rgb(103, 103, 103);}.ld_fancy_heading_6aea90e7df2f2 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e7df2f2\">\n\t<p class=\"lqd-highlight-underline lqd-highlight-grow-left\" data-split-text=\"true\" data-custom-animations=\"true\" data-ca-options='{\"triggerHandler\":\"inview\",\"animationTarget\":\".lqd-lines .split-inner\",\"duration\":700,\"delay\":100,\"easing\":\"easeOutQuint\",\"direction\":\"forward\",\"initValues\":{\"scale\":1},\"animations\":{\"scale\":1}}' data-split-options='{\"type\":\"lines\"}'><span class=\"ld-fh-txt\"> Nos caracterizamos por su enfoque orientado a la eficiencia, la seguridad y el cumplimiento de los m\u00e1s altos est\u00e1ndares ambientales.<\/span><\/p><\/div><style>.ld_spacer_6aea90e7df3f7{height:40px;}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e7df3f7\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1692161875082 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90e7df56d vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90e7df705\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90e7df803 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e7df803\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Akrima<\/strong><br \/>\nRegi\u00f3n de Marrakech-Safi<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90e7df8d9{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e7df8d9\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90e7df966\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e7dfaba\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e7dfbd1\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e7dfbd1\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/111111.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/111111.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/111111-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/111111-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El \u00e1rea de estudio se ubica en la provincia de Jebilet, una zona geol\u00f3gicamente rica y prometedora para la mineralizaci\u00f3n de cobre. Esta mineralizaci\u00f3n est\u00e1 controlada por estructuras como fallas y zonas de cizallamiento, y se manifiesta por vetas de cuarzo y calcita.<\/p>\n<p>El cobre (en forma de malaquita, calcopirita, etc.) se encuentra principalmente en rocas volcano- sedimentarias y esquistosas. Estas caracter\u00edsticas convierten a esta zona en un objetivo privilegiado para la exploraci\u00f3n minera, en particular de metales b\u00e1sicos.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e8037df\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e8038ba\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e8038ba\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>Se identificaron tres estructuras principales, todas consistentes con un modelo de dep\u00f3sito de tipo VMS (sulfuro masivo volcanog\u00e9nico):<\/p>\n<p><strong>&#8211; Estructura 1:<\/strong> Veta de orientaci\u00f3n Este-Oeste, rica en cobre (malaquita, calcopirita, bornita) en una matriz de cuarzo y ankerita.<br \/>\n<strong>&#8211; Estructura 2:<\/strong> Veta de cuarzo oxidado con orientaci\u00f3n norte-sur, conteniendo malaquita dispersa, resultado de procesos de oxidaci\u00f3n secundaria.<br \/>\n<strong>&#8211; Estructura 3:<\/strong> Falla rellena de calcita, que act\u00faa como corredor tect\u00f3nico habiendo favorecido la circulaci\u00f3n de fluidos mineralizantes.alta ley.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e81f01d\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e81f13b\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e81f13b\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"750\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 1000 750&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 1000px) 100vw, 1000px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/DSCN0548.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/DSCN0548.jpg 1000w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/DSCN0548-300x225.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/DSCN0548-16x12.jpg 16w\" data-aspect=\"1.33333333333\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>El estudio geof\u00edsico revel\u00f3 varias anomal\u00edas estructurales interpretadas como vetas o cuerpos intrusivos con alto potencial mineral. Los perfiles analizados muestran zonas de fracturas, engrosamientos y variaciones en el campo geof\u00edsico, lo que indica la probable presencia de vetas ricas en mineral. Tres bloques de anomal\u00edas destacan por su importancia, lo que confirma el gran potencial de la zona para futuras prospecciones y operaciones de perforaci\u00f3n dirigidas.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90e836a29 vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90e836b4f\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90e836c03 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e836c03\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Ighoud<\/strong><br \/>\nRegi\u00f3n de Marrakech-Safi<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90e83737e{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e83737e\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90e837494\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e83762c\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e837763\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e837763\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion77777777.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion77777777.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion77777777-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion77777777-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El permiso de Ighoud se ubica en la compleja y rica regi\u00f3n geol\u00f3gica del Jbilet Occidental. Esta \u00e1rea est\u00e1 compuesta por antiguas formaciones volcanosedimentarias y metam\u00f3rficas, atravesadas por vetas e intrusiones de cuarzo. Contiene varias estructuras mineralizadas de cobre, plomo, zinc y calcita, asociadas con actividad hidrotermal. Este contexto geol\u00f3gico le otorga al permiso un interesante potencial para la mineralizaci\u00f3n de vetas e hidrotermal.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e84f630{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e84f630\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e84f7cd\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e84f8e2\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e84f8e2\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracionggg.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracionggg.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracionggg-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracionggg-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>Dos vetas de cuarzo, Orientadas a N150 y alojadas en esquistos, presentan una mineralizaci\u00f3n significativa de sulfuros de cobre (calcopirita y malaquita). Se muestrearon con un espesor de 30 cm y una extensi\u00f3n de 20 metros.<\/p>\n<p>El an\u00e1lisis de estas muestras es crucial: permitir\u00e1 determinar el contenido de cobre, los elementos asociados y la distribuci\u00f3n espacial de la mineralizaci\u00f3n, evaluando as\u00ed el potencial minero de la regi\u00f3n.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e867d6c{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e867d6c\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e867e82\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e867f3b\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e867f3b\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"750\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 1000 750&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 1000px) 100vw, 1000px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/eeee.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/eeee.jpg 1000w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/eeee-300x225.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/eeee-16x12.jpg 16w\" data-aspect=\"1.33333333333\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>El perfil geof\u00edsico se divide en tres segmentos principales: el primero (0-50 m) presenta una marcada ca\u00edda de la se\u00f1al y revela una zona mineralizada con vetas de mineral y posibles estructuras paralelas; el segundo (50-170 m) presenta una estructura estable y regular; el tercero, particularmente entre 170 y 250 m, se caracteriza por un cambio repentino en la se\u00f1al, lo que indica una zona de contacto o la presencia de un yacimiento mineral, con alteraciones de la roca debidas a intrusiones que permiten modelar zonas ricas. Todo el perfil revela numerosas estructuras paralelas prometedoras, lo que convierte a los sectores 1F200 y 2F200 en objetivos prioritarios para la exploraci\u00f3n.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e880f57{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e880f57\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90e8811ba vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90e881365\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90e881463 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e881463\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Tiouiyine<\/strong><\/p>\n<p>Regi\u00f3n de Draa Tafilalt<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90e881c0a{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e881c0a\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90e881cda\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e881e2d\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e881f66\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e881f66\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion2-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion2-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion2-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion2-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>La zona presenta un contexto geol\u00f3gico complejo, propicio para la mineralizaci\u00f3n. Se caracteriza por:<\/p>\n<ul>\n<li>Diversidad de rocas sedimentarias y volcano-sedimentarias antiguas como andesitas y riolitas y tobas de vetas de microgranito.<br \/>\nNumerosas estructuras tect\u00f3nicas (fallas, pliegues) que canalizaban fluidos mineralizantes.<\/li>\n<li>Una posici\u00f3n de transici\u00f3n entre el Atlas y las mesetas del sur de Marruecos, acentuando esta complejidad.<\/li>\n<li>Una geomorfolog\u00eda accidentada que favorece la erosi\u00f3n y la exposici\u00f3n de rocas potencialmente mineralizadas.<\/li>\n<li>Este conjunto de caracter\u00edsticas crea un ambiente propicio para la formaci\u00f3n de yacimientos.<\/li>\n<\/ul>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e89b976{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e89b976\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e89ba8e\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e89bb72\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e89bb72\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/12-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/12-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/12-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/12-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>Se descubri\u00f3 malaquita, un mineral de cobre, al noroeste del \u00e1rea de estudio. Est\u00e1 asociada con la alteraci\u00f3n hidrotermal en rocas volcano-sedimentarias y vetas de cuarzo.<\/p>\n<p>Su presencia en la superficie indica una zona oxidada, resultante de la alteraci\u00f3n de sulfuros primarios m\u00e1s profundos (como la calcopirita). Esta observaci\u00f3n sugiere la existencia de un sistema mineralizado profundo, controlado por fracturas con orientaci\u00f3n de EO a NE-SO.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e8b3bb9{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e8b3bb9\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e8b3d80\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e8b3ec3\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e8b3ec3\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/fadsadfadfssf.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/fadsadfadfssf.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/fadsadfadfssf-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/fadsadfadfssf-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>El an\u00e1lisis de datos geol\u00f3gicos regionales orient\u00f3 una campa\u00f1a de prospecci\u00f3n espec\u00edfica que arroj\u00f3 resultados concretos y prometedores. Esta campa\u00f1a permiti\u00f3:<\/p>\n<ul>\n<li>La identificaci\u00f3n y ubicaci\u00f3n de vetas de cobre prometedoras.<\/li>\n<li>Mapeo de zonas significativas de alteraci\u00f3n hidrotermal.<\/li>\n<li>El censo de varios \u00edndices de barita<\/li>\n<\/ul>\n<p><strong>Este enfoque met\u00f3dico valid\u00f3 as\u00ed el potencial mineral del sector para este tipo de mineralizaci\u00f3n.<\/strong><\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e8ccb52{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e8ccb52\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90e8ccd46 vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90e8cce89\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90e8ccf2f .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e8ccf2f\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Icht<\/strong><\/p>\n<p>Regi\u00f3n de Souss Massa<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90e8cda59{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e8cda59\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90e8cdb4e\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e8cdce0\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e8cde13\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e8cde13\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/8-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/8-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/8-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/8-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El permiso Icht, ubicado en el Antiatlas sur, se encuentra en una regi\u00f3n con alto potencial metalog\u00e9nico.<\/p>\n<p>Los trabajos de exploraci\u00f3n (mapeo y muestreo) han revelado estructuras mineralizadas (orientadas de este a oeste y de norte a sur) con \u00edndices de cobre, plomo y plata. Estas mineralizaciones, asociadas con la alteraci\u00f3n hidrotermal, son caracter\u00edsticas de los sistemas de vetas del Antiatlas. Por lo tanto, el permiso se considera un entorno geol\u00f3gico prometedor para el descubrimiento de yacimientos de inter\u00e9s econ\u00f3mico.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e8e5810{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e8e5810\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e8e594e\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e8e5a14\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e8e5a14\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/7-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/7-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/7-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/7-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>Una veta de cuarzo oxidado, con un espesor que var\u00eda entre 1 y 3 metros y que se extiende por m\u00e1s deSe ha identificado una veta de 200 metros. Esta veta, orientada principalmente a N110, presenta indicios dispersos de minerales como malaquita, azurita, calcopirita y galena. Estos minerales de oxidaci\u00f3n sugieren una importante actividad mineralizadora en el pasado. La veta tambi\u00e9n fue escenario de antiguas operaciones mineras, como lo demuestra la presencia de un pozo de 15 metros de profundidad y varias trincheras, lo que destaca la importancia hist\u00f3rica de esta estructura para la extracci\u00f3n de minerales valiosos.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e9090c5{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e9090c5\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e9091f6\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e9092b8\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e9092b8\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"396\" height=\"297\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 396 297&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 396px) 100vw, 396px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/a597eee9-a9bf-4368-aae9-dc41e6d1a380.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/a597eee9-a9bf-4368-aae9-dc41e6d1a380.jpg 396w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/a597eee9-a9bf-4368-aae9-dc41e6d1a380-300x225.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/a597eee9-a9bf-4368-aae9-dc41e6d1a380-16x12.jpg 16w\" data-aspect=\"1.33333333333\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>Las labores de exploraci\u00f3n realizadas en el permiso Icht, que incluyeron el muestreo de once muestras de diversas estructuras geol\u00f3gicas y la excavaci\u00f3n de tres trincheras, confirmaron la presencia de mineralizaci\u00f3n de cobre (malaquita y calcopirita) en la veta Cuarzo 1.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e91da7e{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e91da7e\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90e91dc4c vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90e91dd52\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90e91de3b .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e91de3b\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Foum El Hicn<\/strong><\/p>\n<p>Regi\u00f3n de Souss Massa<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90e91e634{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e91e634\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90e91e6ed\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e91e7ef\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e91e8bc\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e91e8bc\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/13-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/13-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/13-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/13-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>Las formaciones geol\u00f3gicas observadas en el \u00e1rea de estudio incluyen calizas metam\u00f3rficas, as\u00ed como calizas dolom\u00edticas ricas en oxidaci\u00f3n. Estas capas se depositan discordantemente sobre un basamento compuesto por lutitas negras y areniscas alternadas. En cuanto a la exploraci\u00f3n minera en el permiso de Foum El Hicn, es fundamental considerar estas diferentes formaciones geol\u00f3gicas.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e93837a{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e93837a\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e9384c2\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e938588\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e938588\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4e3e3d35-bf4e-48ca-832b-86f4b3907d7e.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4e3e3d35-bf4e-48ca-832b-86f4b3907d7e.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4e3e3d35-bf4e-48ca-832b-86f4b3907d7e-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4e3e3d35-bf4e-48ca-832b-86f4b3907d7e-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>El muestreo se centr\u00f3 en varias estructuras mineralizadas reveladoras. Se recolect\u00f3 una veta de calcita y cuarzo con potencial mineralizador, as\u00ed como una muestra en el contacto estrat\u00e9gico entre esquistos negros y calizas dolom\u00edticas para el estudio de interacciones geol\u00f3gicas. Se muestrearon varias vetas de cuarzo mineralizado, que revelaron mineralizaci\u00f3n de sulfuro, malaquita y calcopirita, incluyendo una prometedora asociaci\u00f3n de mineralizaci\u00f3n de plata con cobre. Una muestra particularmente significativa mostr\u00f3 una alta concentraci\u00f3n de malaquita y calcopirita, lo que confirma la presencia de una mineralizaci\u00f3n sustancial en la zona.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e950802{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e950802\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e950923\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e9509df\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e9509df\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion4444.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion4444.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion4444-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion4444-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La campa\u00f1a de exploraci\u00f3n comenz\u00f3 con la recopilaci\u00f3n y compilaci\u00f3n de datos de referencia, incluyendo mapas e informes geol\u00f3gicos existentes. Continu\u00f3 con un mapeo geol\u00f3gico detallado de campo, centr\u00e1ndose en la observaci\u00f3n de afloramientos y estudios de zonas de contacto. El muestreo selectivo result\u00f3 en la recolecci\u00f3n de cinco muestras representativas de formaciones espec\u00edficas: una veta de calcita con cuarzo, un contacto entre esquistos y calizas, y vetas de cuarzo con malaquita, calcopirita y sulfuros. Estas muestras se someter\u00e1n a exhaustivos an\u00e1lisis de laboratorio (mineral\u00f3gicos y geoqu\u00edmicos) para determinar las concentraciones de metales. Paralelamente, se excavar\u00e1n zanjas de exploraci\u00f3n para exponer estructuras en profundidad, todo lo cual se guiar\u00e1 por una evaluaci\u00f3n ambiental continua para garantizar pr\u00e1cticas sostenibles y minimizar el impacto ecol\u00f3gico.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e96736e{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e96736e\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90e96759d vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90e9676fe\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90e96779b .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e96779b\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Tizounine<\/strong><\/p>\n<p>Regi\u00f3n de Souss Massa<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90e967f6f{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e967f6f\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90e967ff8\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e9680bc\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e968187\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e968187\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/3-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/3-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/3-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/3-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El permiso de estudio se ubica en el Jbel Guilez, un macizo perteneciente a la cadena herc\u00ednica del Antiatlas marroqu\u00ed. Esta regi\u00f3n es reconocida por su potencial metalog\u00e9nico, confirmado por la presencia de \u00edndices polimet\u00e1licos. La zona se caracteriza por la mineralizaci\u00f3n de plomo y cobre, materializada por vetas de cuarzo e impregnaciones en las rocas sedimentarias de la formaci\u00f3n Ktaoua.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e97e632{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e97e632\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e97e74c\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e97e80e\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e97e80e\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/fff.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/fff.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/fff-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/fff-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>Resultados de muestreo y formaciones mineralizadas:<\/p>\n<p>&#8211; Cuarzo con \u00f3xidos de hierro y trazas de plomo (Pb): Una serie de muestras revel\u00f3 inclusiones de plomo en una matriz de cuarzo y \u00f3xido de hierro. Esta asociaci\u00f3n es consistente con la mineralizaci\u00f3n polimet\u00e1lica de los sistemas VMS, donde el plomo se encuentra com\u00fanmente junto con el cobre y el zinc.<br \/>\n&#8211; Cuarzo con \u00f3xidos de hierro y trazas de malaquita: Las muestras de zonas oxidadas muestran la presencia de malaquita, un carbonato secundario de cobre. Esta mineralizaci\u00f3n refleja procesos de oxidaci\u00f3n y enriquecimiento sup\u00e9rgeno, t\u00edpicamente superpuestos a la mineralizaci\u00f3n primaria de tipo VMS.<\/p>\n<p>&#8211; Cuarzo, \u00f3xidos de hierro y trazas de plomo y plata: Finalmente, algunas formaciones revelan la coexistencia de cuarzo, \u00f3xidos de hierro y trazas de plomo, lo que confirma la heterogeneidad mineral\u00f3gica y la complejidad geoqu\u00edmica del \u00e1rea explorada.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e994cf5{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e994cf5\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e994e29\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e994eed\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e994eed\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion555.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion555.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion555-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion555-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>Los trabajos de prospecci\u00f3n realizados en el permiso Tizounine revelaron la presencia de vetas mineralizadas, que fueron objeto de operaciones sistem\u00e1ticas de reconocimiento y delimitaci\u00f3n. Estas intervenciones combinaron t\u00e9cnicas de excavaci\u00f3n ligera (raspado, desbroce) y pesada (zanjas de reconocimiento, trabajos de explotaci\u00f3n), lo que permiti\u00f3 precisar la continuidad geom\u00e9trica y la<br \/>\ndistribuci\u00f3n espacial de las estructuras mineralizadas identificadas. Direcci\u00f3n NS (potencia media 40com y vetas de cuarzo). \u00cdndices de plomo.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e9ac980{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e9ac980\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90e9acbfe vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90e9acda5\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90e9aceb3 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e9aceb3\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Akka<\/strong><\/p>\n<p>Regi\u00f3n de Souss Massa<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90e9ad7bf{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e9ad7bf\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90e9ad8c8\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e9adaa9\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e9adbdb\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e9adbdb\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/11-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/11-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/11-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/11-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El \u00e1rea de estudio, ubicada en la regi\u00f3n occidental del Antiatlas, cerca de la ciudad de Akka, presenta un notable sistema de mineralizaci\u00f3n hidrotermal. Esta mineralizaci\u00f3n se manifiesta mediante una red de vetas de calcita, cuya morfolog\u00eda y contexto geol\u00f3gico proporcionan valiosas pistas sobre las condiciones de su formaci\u00f3n.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e9c55db{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e9c55db\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e9c575c\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e9c5856\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e9c5856\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/sdfaserewr.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/sdfaserewr.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/sdfaserewr-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/sdfaserewr-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p><strong>Las formaciones geol\u00f3gicas del \u00e1rea de estudio incluyen:<\/strong><br \/>\n&#8211; Caliza altamente deformada cortada por vetas de calcita;<br \/>\n&#8211; Caliza altamente deformada cortada por vetas de calcita y rica en \u00f3xido de hierro.<br \/>\n&#8211; Caliza altamente deformada cortada por vetas de calcita, rica en \u00f3xido de hierro y que contiene f\u00f3siles;Las vetas de cuarzo se intercalan dentro de formaciones de arenisca y esquisto; este entorno estructural es un control conocido para la mineralizaci\u00f3n de plomo.<br \/>\n&#8211; Vetas de cuarzo con manchas de plomo que corren paralelas a la formaci\u00f3n; vetas de cuarzo alojadas en formaciones de arenisca que contienen lumachels; vetas de cuarzo oxidado dentro de formaciones de arenisca y esquisto.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e9dd0e2{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e9dd0e2\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90e9dd20c\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90e9dd2d2\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90e9dd2d2\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/06ed63a9-6f25-4c49-931f-f39c810099af.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/06ed63a9-6f25-4c49-931f-f39c810099af.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/06ed63a9-6f25-4c49-931f-f39c810099af-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/06ed63a9-6f25-4c49-931f-f39c810099af-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La exploraci\u00f3n del permiso Akka se estructur\u00f3 en torno a un mapeo geol\u00f3gico detallado, que sirvi\u00f3 como base metodol\u00f3gica para guiar las campa\u00f1as de prospecci\u00f3n y muestreo. Este enfoque permiti\u00f3 localizar e identificar varias vetillas de cuarzo con evidencia significativa de mineralizaci\u00f3n de plomo.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90e9f3848{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90e9f3848\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90e9f3a5a vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90e9f3bb9\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90e9f3c69 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90e9f3c69\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Ain Zohra<\/strong><\/p>\n<p>Regi\u00f3n de Oujda<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90ea00370{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ea00370\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90ea00441\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ea00599\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ea006a5\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ea006a5\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion33.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion33.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion33-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion33-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El \u00e1rea de estudio presenta una diversidad de formaciones geol\u00f3gicas caracter\u00edsticas de ambientes \u00e1ridos a semi\u00e1ridos. Se encuentran principalmente evaporitas (como yeso y halita), formadas por precipitaci\u00f3n, y arcillas rojas yes\u00edferas, ricas en yeso. Estas formaciones, con colores distintivos (rojo, amarillento, verde), son resultado de procesos de evaporaci\u00f3n, alteraci\u00f3n qu\u00edmica y erosi\u00f3n, y desempe\u00f1an un papel fundamental en la composici\u00f3n del paisaje geol\u00f3gico local.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ea17898{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ea17898\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ea17a3b\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ea17b79\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ea17b79\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat2.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat2.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat2-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat2-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>La secuencia sedimentaria descrita es caracter\u00edstica de una cuenca de tipo evapor\u00edtico, formada en condiciones clim\u00e1ticas \u00e1ridas a semi\u00e1ridas. El conjunto litol\u00f3gico, junto con la menci\u00f3n de una presencia de litio, revela un entorno deposicional controlado y potencial econ\u00f3mico para elementos cr\u00edticos.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ea2ef45{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ea2ef45\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ea2f0b8\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ea2f22b\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ea2f22b\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"1515\" height=\"1010\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 1515 1010&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 1515px) 100vw, 1515px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Ain-zohra-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Ain-zohra-1.jpg 1515w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Ain-zohra-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Ain-zohra-1-1024x683.jpg 1024w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Ain-zohra-1-18x12.jpg 18w\" data-aspect=\"1.5\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La exploraci\u00f3n se ha centrado espec\u00edficamente en dos formaciones geol\u00f3gicas de inter\u00e9s econ\u00f3mico: formaciones arcillosas salinas y margas yes\u00edferas. Esta metodolog\u00eda garantiza una evaluaci\u00f3n fiable de la composici\u00f3n y el potencial mineral de los materiales muestreados.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ea48931{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ea48931\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90ea48b26 vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90ea48c69\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90ea48d58 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90ea48d58\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Guercif<\/strong><\/p>\n<p>Regi\u00f3n de Oujda<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90ea494d9{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ea494d9\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90ea495a0\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ea4969f\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ea49772\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ea49772\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion66.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion66.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion66-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/goliat-minerals-marruecos-minas-exploracion66-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>La cuenca de Guercif constituye la parte oriental del Corredor del Rif Sur, una gran depresi\u00f3n situada entre el dominio intracontinental de la Meseta marroqu\u00ed al sur y la cordillera del Rif al norte. La cuenca est\u00e1 rellena por una gruesa secuencia (de varios kil\u00f3metros) de sedimentos de edad ne\u00f3gena a cuaternaria (desde -23 millones de a\u00f1os). Estos sedimentos son principalmente:<\/p>\n<ul>\n<li>Conglomerados (piedras pudines), testigos de la r\u00e1pida erosi\u00f3n de la naciente cadena del Rif.<\/li>\n<li>Areniscas y arcillas, depositadas en ambientes aluviales, lacustres y deltaicos.<\/li>\n<li>Margas y evaporitas (yeso), indicativas de episodios de confinamiento y desecaci\u00f3n.<\/li>\n<\/ul>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ea61871{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ea61871\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ea619d4\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ea61aae\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ea61aae\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"1558\" height=\"1039\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 1558 1039&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 1558px) 100vw, 1558px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Guercif-Mineralisation.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Guercif-Mineralisation.jpg 1558w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Guercif-Mineralisation-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Guercif-Mineralisation-1024x683.jpg 1024w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/Guercif-Mineralisation-18x12.jpg 18w\" data-aspect=\"1.49951876805\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>El macizo Tri\u00e1sico de la regi\u00f3n de Uchda, compuesto de yeso y sal, es muy susceptible a la disoluci\u00f3n. Esto provoca una intensa actividad k\u00e1rstica, que provoca una extensa evoluci\u00f3n del relieve, derrumbes y la formaci\u00f3n repentina de grandes dolinas y sumideros. Este proceso crea paisajes ca\u00f3ticos donde se producen simult\u00e1neamente diversos derrumbes de laderas (deslizamientos de tierra, desprendimientos de rocas). En la base de estas laderas se forman conos aluviales arcillo- salinos, identificados como posibles trampas para el enriquecimiento de litio derivado de la meteorizaci\u00f3n de las rocas salinas.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ea7d155{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ea7d155\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ea7d28a\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ea7d346\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ea7d346\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15ce802b-ca1e-49ac-9076-10d315628b91.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15ce802b-ca1e-49ac-9076-10d315628b91.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15ce802b-ca1e-49ac-9076-10d315628b91-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15ce802b-ca1e-49ac-9076-10d315628b91-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La exploraci\u00f3n comenz\u00f3 con un mapeo geol\u00f3gico y estructural preliminar para identificar las principales unidades litol\u00f3gicas y estructuras (fallas, pliegues) que influyen en la mineralizaci\u00f3n. Sobre esta base, se planific\u00f3 un programa de campo detallado, definiendo los objetivos prioritarios y los m\u00e9todos de investigaci\u00f3n.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ea95edc{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ea95edc\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90ea96133 vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90ea9629d\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90ea9636e .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90ea9636e\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Ain Zelfoune<\/strong><\/p>\n<p>Regi\u00f3n de Fez-Mequinez<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90ea96c99{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ea96c99\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90ea96d6d\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ea96ed0\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ea97014\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ea97014\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/9f0c8bdf-6e43-4c4c-8be9-5355daa40c30.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/9f0c8bdf-6e43-4c4c-8be9-5355daa40c30.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/9f0c8bdf-6e43-4c4c-8be9-5355daa40c30-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/9f0c8bdf-6e43-4c4c-8be9-5355daa40c30-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La campa\u00f1a de exploraci\u00f3n realizada en la zona ha identificado y localizado varias formaciones sedimentarias de inter\u00e9s. Entre ellas, se ha prestado especial atenci\u00f3n a las formaciones arcillosas salinas de color rojo y a las margas. Estas unidades litol\u00f3gicas, cuya caracterizaci\u00f3n detallada se encuentra actualmente en curso, son de gran inter\u00e9s por su potencial en minerales industriales y por su papel en la comprensi\u00f3n de la evoluci\u00f3n geol\u00f3gica de la cuenca sedimentaria.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eaaf830{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eaaf830\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90eaafa41 vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90eaafbbb\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90eaafcab .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90eaafcab\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>El Ksabi<\/strong><\/p>\n<p>Regi\u00f3n de Fez-Mequinez<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90eab06e8{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eab06e8\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90eab07ca\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eab0931\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eab0a62\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eab0a62\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"1152\" height=\"864\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 1152 864&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 1152px) 100vw, 1152px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/DSCN0383.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/DSCN0383.jpg 1152w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/DSCN0383-300x225.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/DSCN0383-1024x768.jpg 1024w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/DSCN0383-16x12.jpg 16w\" data-aspect=\"1.33333333333\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La campa\u00f1a de exploraci\u00f3n realizada en la zona ha identificado y localizado varias formaciones sedimentarias de inter\u00e9s. Entre ellas, se ha prestado especial atenci\u00f3n a las formaciones arcillosas salinas de color rojo y a las margas. Estas unidades litol\u00f3gicas, cuya caracterizaci\u00f3n detallada se encuentra actualmente en curso, son de gran inter\u00e9s por su potencial en minerales industriales y por su papel en la comprensi\u00f3n de la evoluci\u00f3n geol\u00f3gica de la cuenca sedimentaria.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eac998d{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eac998d\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90eac9b2d vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90eac9c46\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90eac9cfb .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90eac9cfb\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Qelaat M\u00b4gouna<\/strong><\/p>\n<p>Regi\u00f3n de Draa Tafilalt<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90eaca5bc{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eaca5bc\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90eaca6a1\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eaca7dd\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eaca8c6\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eaca8c6\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"433\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 433&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15e140de-fccc-4501-9ac8-5e273ef4111f.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15e140de-fccc-4501-9ac8-5e273ef4111f.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15e140de-fccc-4501-9ac8-5e273ef4111f-300x156.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/15e140de-fccc-4501-9ac8-5e273ef4111f-18x9.jpg 18w\" data-aspect=\"1.92378752887\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>La regi\u00f3n de Qelaat M\u00b4Gouna, en la cordillera oriental del Antiatlas, presenta un contexto geol\u00f3gico complejo, marcado por una estructura interna prec\u00e1mbrica. Su historia geol\u00f3gica se caracteriza por dos ciclos principales: un primer ciclo que comprende magmatismo calcoalcalino \u00e1cido y deposici\u00f3n en una<br \/>\ncuenca de arco, seguido de un segundo ciclo de formaciones volcanocl\u00e1sticas y plut\u00f3nicas. Esta evoluci\u00f3n, influenciada por fases de subducci\u00f3n, rifting y deformaci\u00f3n panafricana, molde\u00f3 un basamento volcanosedimentario intruido por granitos y gabros. Esta complejidad geol\u00f3gica es fundamental para comprender la din\u00e1mica. potencial regional y de recursos minerales.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eae49fd{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eae49fd\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eae4b32\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eae4c16\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eae4c16\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/14.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/14.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/14-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/14-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>La exploraci\u00f3n ha revelado la presencia de diversas formaciones geol\u00f3gicas, incluyendo calizas amarillentas ligeramente dolom\u00edticas, arcillas rojizas con vetas de yeso y pelitas negras ricas en \u00f3xidos de hierro. Estas formaciones muestran indicios prometedores de mineralizaci\u00f3n, especialmente de plomo y plata.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eb09c09{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eb09c09\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eb09d8a\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eb09ea9\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eb09ea9\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5e5b69d0-5235-44d8-96c9-6674d17213fc.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5e5b69d0-5235-44d8-96c9-6674d17213fc.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5e5b69d0-5235-44d8-96c9-6674d17213fc-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5e5b69d0-5235-44d8-96c9-6674d17213fc-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La campa\u00f1a de exploraci\u00f3n realizada en el permiso de <strong>Qelaat M\u00b4gouna<\/strong> result\u00f3 en la recolecci\u00f3n de muestras representativas, tomadas mediante una cuadr\u00edcula que abarcaba alrededor de diez puntos de inter\u00e9s geol\u00f3gico. Esta estrategia de muestreo investig\u00f3 sistem\u00e1ticamente tres unidades litol\u00f3gicas principales:<\/p>\n<p>&#8211; Calizas amarillentas con bajo contenido de dolomita, que proporcionan indicadores clave de la composici\u00f3n mineral\u00f3gica de la cuenca.<br \/>\n&#8211; Formaciones de arcilla rojiza atravesadas por vetas de yeso, testimonio de procesos diagen\u00e9ticos y sedimentarios distintivos.<br \/>\n&#8211; Pelitas negras con alta concentraci\u00f3n de \u00f3xidos de hierro, cuyo origen y g\u00e9nesis son de gran inter\u00e9s para el modelado de sistemas mineralizantes regionales.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eb21a90{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eb21a90\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90eb21cba vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90eb21e84\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90eb21f89 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90eb21f89\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Cinco Permisos de exploraci\u00f3n Zagora: <\/strong><\/p>\n<p>4 Permisos y 1 Licencia<\/p>\n<p>Regi\u00f3n de Draa Tafilalt<\/span><\/h3><\/div>\n\t<div class=\"wpb_text_column wpb_content_element\" >\n\t\t<div class=\"wpb_wrapper\">\n\t\t\t<p>NB: El Ministerio de Transici\u00f3n Energ\u00e9tica y Desarrollo Sostenible de Marruecos otorg\u00f3 recientemente todos estos permisos a la empresa como parte del programa nacional de reasignaci\u00f3n de permisos y licencias mineras. La superficie total abarca 96 kil\u00f3metros cuadrados, de los cuales 16 corresponden a las licencias.<\/p>\n\n\t\t<\/div>\n\t<\/div>\n<style>@media (min-width: 992px) { .ld_spacer_6aea90eb22799{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eb22799\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90eb22835\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eb228f9\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eb2299f\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eb2299f\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El \u00e1rea de estudio se ubica en la parte sureste del interior de Bou Azzer (Antiatlas Central), m\u00e1s precisamente a nivel de su cobertura paleozoica. Localmente, el sector se caracteriza por formaciones de arenisca-esquistosa a arenisca-caliza de edad Adoudoniana a C\u00e1mbrico Medio. Desde un punto de vista estructural, el per\u00edmetro est\u00e1 afectado por un sistema de fallas multidireccionales, principalmente orientadas al este-oeste, noroeste-sureste y noreste-suroeste.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eb3ab83{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eb3ab83\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eb3ad03\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eb3ae29\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eb3ae29\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5ca64dd9-63e7-4da8-b77b-a00f8dfe7d45.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5ca64dd9-63e7-4da8-b77b-a00f8dfe7d45.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5ca64dd9-63e7-4da8-b77b-a00f8dfe7d45-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5ca64dd9-63e7-4da8-b77b-a00f8dfe7d45-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>Un entorno geol\u00f3gico favorable con rocas hu\u00e9sped de arenisca y arenisca calc\u00e1rea contiene varias estructuras mineralizadas en los cuatro permisos. Estas consisten en vetas, capas y vetillas de barita de alta calidad que contienen agregados de plomo, lo que demuestra el potencial de una mineralizaci\u00f3n sustancial de barita.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eb5427a{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eb5427a\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eb543a7\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eb5446e\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eb5446e\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/8bf02744-c337-461e-982a-dc7bfd9e494f.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/8bf02744-c337-461e-982a-dc7bfd9e494f.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/8bf02744-c337-461e-982a-dc7bfd9e494f-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/8bf02744-c337-461e-982a-dc7bfd9e494f-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La exploraci\u00f3n de los permisos de Zagora se llev\u00f3 a cabo mediante una metodolog\u00eda integrada basada en una extensa investigaci\u00f3n bibliogr\u00e1fica y la observaci\u00f3n directa de campo para la interpretaci\u00f3n geol\u00f3gica. Este enfoque estrat\u00e9gico permiti\u00f3 el mapeo detallado de varios yacimientos mineralizados (principalmente barita y plomo). La correlaci\u00f3n entre los objetivos identificados durante la fase preliminar y las observaciones de campo confirma el potencial mineralizado del distrito, posicionando a la barita como un objetivo econ\u00f3mico prioritario que justifica la continuaci\u00f3n de las investigaciones geol\u00f3gicas.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eb6c43d{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eb6c43d\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90eb6c6ad vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90eb6c898\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90eb6c993 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90eb6c993\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Bourbia<\/strong><\/p>\n<p>Regi\u00f3n de Draa Tafilalt<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90eb6d1ba{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eb6d1ba\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90eb6d284\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eb6d47e\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eb6d5c6\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eb6d5c6\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"769\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 769 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 769px) 100vw, 769px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/37e4059c-b284-4f1d-a62d-27469d55afb4.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/37e4059c-b284-4f1d-a62d-27469d55afb4.jpg 769w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/37e4059c-b284-4f1d-a62d-27469d55afb4-300x217.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/37e4059c-b284-4f1d-a62d-27469d55afb4-18x12.jpg 18w\" data-aspect=\"1.38558558559\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El \u00e1rea de estudio se ubica en el Anti-atlas, una vasta estructura anticlinal con orientaci\u00f3n ENE-OSW. El permiso presenta una secuencia geol\u00f3gica completa que comprende formaciones desde el Prec\u00e1mbrico Tard\u00edo hasta el C\u00e1mbrico, con dep\u00f3sitos cuaternarios superpuestos. Las unidades prec\u00e1mbricas (grupo PIII), compuestas por ignimbritas, andesitas, traquitas y sedimentos volcanodetr\u00edticos, representan un registro clave de la historia geol\u00f3gica regional.<\/p>\n<p>El estudio de estas formaciones es de fundamental importancia para comprender la evoluci\u00f3n geodin\u00e1mica de la regi\u00f3n, evaluar su potencial de recursos minerales e identificar peligros geol\u00f3gicos, permitiendo as\u00ed una gesti\u00f3n optimizada de los recursos naturales.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eb85e4e{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eb85e4e\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eb85f7d\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eb86042\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eb86042\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6ad3ecd3-1cfe-4676-9794-1993c0156258.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6ad3ecd3-1cfe-4676-9794-1993c0156258.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6ad3ecd3-1cfe-4676-9794-1993c0156258-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6ad3ecd3-1cfe-4676-9794-1993c0156258-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p><strong>Arenisca cuarzosa ferruginosa:<\/strong> Estas formaciones se caracterizan por un alto contenido de cuarzo y\u00f3xidos de hierro, lo que indica condiciones <strong>deposicionales ricas en hierro.<\/strong><\/p>\n<p><strong>Cuarzo asociado con cuarcita que contiene trazas de \u00f3xidos de hierro:<\/strong> Las muestras muestran una asociaci\u00f3n \u00edntima entre el cuarzo y la cuarcita, con trazas de \u00f3xidos de hierro que sugieren mineralizaci\u00f3n secundaria.<\/p>\n<p><strong>Caliza margosa amarillenta:<\/strong> Se identifica por su tono amarillento debido a inclusiones de arcilla y hierro, lo que sugiere ambientes deposicionales mixtos.<\/p>\n<p><strong>Terrenos ricos en hierro:<\/strong> Estos terrenos presentan una alta concentraci\u00f3n de minerales ferruginosos, lo que indica una fuente significativa de hierro.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eb9ec6e{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eb9ec6e\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90eb9ee0a\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90eb9ef38\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90eb9ef38\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4d99a358-a019-4ef0-befa-43833c90bcda.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4d99a358-a019-4ef0-befa-43833c90bcda.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4d99a358-a019-4ef0-befa-43833c90bcda-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4d99a358-a019-4ef0-befa-43833c90bcda-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La campa\u00f1a de exploraci\u00f3n en el permiso BOURBIAA comenz\u00f3 con un mapeo detallado que revel\u00f3 una notable diversidad litol\u00f3gica, dominada por areniscas de cuarzo y cuarcitas. Se tomaron once muestras representativas de estas formaciones con variado potencial mineral\u00f3gico. Para la siguiente fase, se planea excavar trincheras para investigar sistem\u00e1ticamente las \u00e1reas objetivo, incluyendo en particular las areniscas de cuarzo ricas en \u00f3xidos de hierro, los terrenos ferruginosos, las calizas margosas y las vetas de cuarzo.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ebb8a92{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ebb8a92\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90ebb8c97 vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90ebb8da0\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90ebb8e81 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90ebb8e81\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Boughrar<\/strong><\/p>\n<p>Regi\u00f3n de Draa Tafilalt<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90ebb9834{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ebb9834\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90ebb98d6\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ebb99f8\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ebb9ab6\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ebb9ab6\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"721\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 721 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 721px) 100vw, 721px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/2b75a09c-14e2-4be0-840a-c6d9e63f36d6.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/2b75a09c-14e2-4be0-840a-c6d9e63f36d6.jpg 721w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/2b75a09c-14e2-4be0-840a-c6d9e63f36d6-300x231.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/2b75a09c-14e2-4be0-840a-c6d9e63f36d6-16x12.jpg 16w\" data-aspect=\"1.2990990991\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>La propiedad Boughrar, ubicada en el enclave prec\u00e1mbrico de Tifernine, presenta un entorno geol\u00f3gico dominado por rocas volc\u00e1nicas del Grupo Ouarzazate (Prec\u00e1mbrico III). La mineralizaci\u00f3n de cobre y hierro-manganeso se concentra en las zonas central y meridional, asociada a andesitas porf\u00eddicas (Formaci\u00f3n Boughrar) y riolitas masivas (Formaci\u00f3n Wayt Az-Zig). La zona norte, compuesta por rocas sedimentarias cl\u00e1sticas del Grupo Tata (Infrac\u00e1mbrico-C\u00e1mbrico), permanece est\u00e9ril.<\/p>\n<p>La propiedad est\u00e1 intersectada por diques m\u00e1ficos y f\u00e9lsicos, as\u00ed como vetas de cuarzo, generalmente sin mineralizar en la superficie. Los datos sugieren un abultamiento estructural con direcci\u00f3n ONO.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ebd0ee2{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ebd0ee2\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ebd1082\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ebd11b5\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ebd11b5\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5cc81097-063f-4afa-97e8-492f72baeb36.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5cc81097-063f-4afa-97e8-492f72baeb36.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5cc81097-063f-4afa-97e8-492f72baeb36-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/5cc81097-063f-4afa-97e8-492f72baeb36-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>La licencia de Boughrar se caracteriza por formaciones volc\u00e1nicas, principalmente riolitas, que albergan un yacimiento de cobre y plata. La mineralizaci\u00f3n, concentrada en el sector sureste de la licencia, se asocia con estructuras de inclinaci\u00f3n pronunciada, con direcci\u00f3n este-oeste a noreste. Estas incluyen diques \u00edgneos de composici\u00f3n diversa, a menudo bordeados por vetas mineralizadas, y, subordinadamente, vetas independientes de los diques.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ebe9c54{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ebe9c54\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ebe9d69\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ebe9e2f\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ebe9e2f\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"781\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 781 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 781px) 100vw, 781px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/1a08acf3-a513-4e0e-af14-b2687c05c22d.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/1a08acf3-a513-4e0e-af14-b2687c05c22d.jpg 781w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/1a08acf3-a513-4e0e-af14-b2687c05c22d-300x213.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/1a08acf3-a513-4e0e-af14-b2687c05c22d-18x12.jpg 18w\" data-aspect=\"1.40720720721\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>Una campa\u00f1a geof\u00edsica realizada en varias \u00e1reas del permiso incluy\u00f3 la adquisici\u00f3n de siete perfiles con antenas de 600 MHz, lo que permiti\u00f3 la identificaci\u00f3n de posibles vetas de cobre.<\/p>\n<p>La interpretaci\u00f3n distingui\u00f3 vetas mineralizadas de roca est\u00e9ril, confirm\u00f3 la geometr\u00eda de un dique atravesado por el perfil 1C200 y revel\u00f3 varias vetas secundarias prometedoras en los perfiles 2A200, 1A200 y 3A200. La integraci\u00f3n de los datos en un SIG proporcion\u00f3 un modelo preciso de la direcci\u00f3n y magnitud del cuerpo mineral principal, as\u00ed como tres nuevas estructuras similares con potencial comprobado.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ec0e03d{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ec0e03d\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90ec0e265 vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90ec0e409\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90ec0e51c .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90ec0e51c\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Tikirt<\/strong><\/p>\n<p>Regi\u00f3n de Draa Tafilalt<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90ec0ed6a{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ec0ed6a\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90ec0eea3\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ec0f0aa\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ec0f1c3\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ec0f1c3\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"477\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 477 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 477px) 100vw, 477px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/0b15579b-196e-461b-be83-f57cf20117ee.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/0b15579b-196e-461b-be83-f57cf20117ee.jpg 477w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/0b15579b-196e-461b-be83-f57cf20117ee-258x300.jpg 258w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/0b15579b-196e-461b-be83-f57cf20117ee-10x12.jpg 10w\" data-aspect=\"0.859459459459\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El entorno geol\u00f3gico de la concesi\u00f3n de Ouarzazate se caracteriza por la presencia de diques m\u00e1ficos e intrusiones magm\u00e1ticas que atraviesan un complejo basamento metam\u00f3rfico. Estas formaciones geol\u00f3gicas son t\u00edpicas de la regi\u00f3n y suelen estar asociadas a fracturas en la roca madre, lo que favorece la mineralizaci\u00f3n. Los diques, generalmente orientados de este a oeste, presentan indicios de cobre con buzamiento suave y yacimientos de manganeso en la parte sur de la concesi\u00f3n, lo que sugiere un considerable potencial mineral. La concesi\u00f3n de Ouarzazate se caracteriza por una gran diversidad geol\u00f3gica, lo que refleja un s\u00f3lido potencial de exploraci\u00f3n y miner\u00eda. El trabajo de campo realizado en la regi\u00f3n incluye cartograf\u00eda geol\u00f3gica detallada y muestreo selectivo de rocas de diversas facies.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ec29bca{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ec29bca\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ec29d79\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ec29e70\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ec29e70\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/4-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>Las unidades litol\u00f3gicas expuestas en esta \u00e1rea consisten en formaciones volc\u00e1nicas, volcano- sedimentarias y sedimentarias, que abarcan un rango de edad desde el Neoproterozoico hasta el Cuaternario. Esta diversidad geol\u00f3gica confiere a la regi\u00f3n un alto potencial mineral\u00f3gico, ilustrado por la presencia de varios dep\u00f3sitos y ocurrencias de manganeso (Mn), hierro (Fe) y cobre (Cu). La mineralizaci\u00f3n es principalmente del tipo VMS (Sulfuro Masivo Vulcanog\u00e9nico), un estilo reconocido mundialmente por su importancia econ\u00f3mica, caracterizado por concentraciones de metales formadas en asociaci\u00f3n con la actividad volc\u00e1nica y ambientes hidrotermales. Dada esta diversidad litol\u00f3gica y el contexto favorable, el contenido mineral es&#8230; considerado significativo, reforzando el inter\u00e9s de esta \u00e1rea para la exploraci\u00f3n en la forma<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ec44275{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ec44275\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ec44418\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ec44539\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ec44539\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/16.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/16.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/16-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/16-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>Una campa\u00f1a geof\u00edsica realizada en el permiso permiti\u00f3 la adquisici\u00f3n de perfiles perpendiculares a los probables ejes de mineralizaci\u00f3n, revelando varias estructuras significativas. El perfil 2D200, que intersecta una falla y una veta de cobre, identific\u00f3 siete anomal\u00edas estructuradas en tres bloques: uno (10-25 m) interpretado como una falla, y otros dos (40-200 m y 205-265 m) que indican alteraci\u00f3n asociada a materiales intrusivos. Estas anomal\u00edas muestran una buena correlaci\u00f3n con los afloramientos de cobre, una consistencia que tambi\u00e9n se observa en los perfiles 3D200 y 5D200; este \u00faltimo revela profundas modificaciones tect\u00f3nicas. Finalmente, el perfil 4D200 destac\u00f3 anomal\u00edas distintivas en los contactos intrusivos a 5 y 50 metros.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ec5b633{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ec5b633\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1759482521938 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90ec5b878 vc_row-has-fill vc_row-has-bg\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-6aea90ec5ba17\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90ec5bb09 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading ld_fancy_heading_6aea90ec5bb09\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" ><span class=\"ld-fh-txt\"> <strong>Tinzoulin<\/strong><\/p>\n<p>Regi\u00f3n de Draa Tafilalt<\/span><\/h3><\/div><style>@media (min-width: 992px) { .ld_spacer_6aea90ec5c772{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ec5c772\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90ec5c867\"><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ec5c9c2\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ec5cae3\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ec5cae3\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6-1.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6-1.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6-1-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/6-1-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Geolog\u00eda<\/h3>\t\t\t<p>El \u00e1rea de estudio pertenece geol\u00f3gicamente a la parte sureste del inlier de Bou Azzer, exactamente sobre la cubierta paleozoica. Este inlier forma parte del Anti Atlas Central. El inlier de Bou Azzer aflora en forma de un complejo ofiol\u00edtico y un complejo de arcos a la altura del accidente principal del Anti Atlas. Localmente, el per\u00edmetro de los permisos est\u00e1 ocupado por las facies de la cubierta paleozoica, manifestada por terrenos que datan del Adoudoniano al C\u00e1mbrico Medio. La litolog\u00eda predominante en el \u00e1rea de estudio se presenta en formaciones de arenisca-esquistosa a arenisca-caliza.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ec74b5f{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ec74b5f\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ec74cf9\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ec74e18\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ec74e18\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/122.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/122.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/122-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/122-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Mineralizaci\u00f3n<\/h3>\t\t\t<p>Dentro de la licencia, se mapearon tres estructuras de barita como vetas, largueros y estratos estratiformes. Tambi\u00e9n se identificaron dos nuevas vetas de barita, adem\u00e1s de un gran afloramiento carbonatado cortado por largueros de cuarzo.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90ec8dcc5{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90ec8dcc5\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-4 liquid-column-6aea90ec8dde2\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><div id=\"ld_content_box_6aea90ec8deda\" class=\"fancy-box fancy-box-classic ld_content_box_6aea90ec8deda\">\n\t\n\t<div class=\"cb-img-container mb-4\">\n\n\t\t<figure class=\"fancy-box-image\"><img loading=\"lazy\" decoding=\"async\" width=\"833\" height=\"555\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 833 555&#039;%2F&gt;\" class=\"attachment-full size-full ld-lazyload\" alt=\"\" srcset=\"\" sizes=\"auto, (max-width: 833px) 100vw, 833px\" data-src=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/16.jpg\" data-srcset=\"https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/16.jpg 833w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/16-300x200.jpg 300w, https:\/\/www.goliatminerals.com\/wp-content\/uploads\/2025\/10\/16-18x12.jpg 18w\" data-aspect=\"1.5009009009\" \/><\/figure>\t\t\t\t\n\t\t\n\t<\/div><!-- \/.cb-img-container -->\n\n\t<div class=\"fancy-box-contents\">\n\t\t\n\t\t<div class=\"fancy-box-header\">\n\t\t\t<h3>Exploraci\u00f3n<\/h3>\t\t\t<p>La exploraci\u00f3n de la licencia Tinzouline se gui\u00f3 por un enfoque met\u00f3dico, comenzando con la creaci\u00f3n de un mapa predictivo de \u00edndices geol\u00f3gicos antes del inicio del trabajo de campo. Esta planificaci\u00f3n permiti\u00f3 la identificaci\u00f3n y documentaci\u00f3n precisa de numerosos yacimientos minerales, incluyendo un extenso sistema de vetillas, vetas bien individualizadas y varios niveles bar\u00edticos estratiformes.<\/p>\n<p>La consistencia entre los objetivos definidos en la fase preparatoria y los descubrimientos en campo confirman el potencial mineralizante del \u00e1rea, estableciendo a la barita como un recurso econ\u00f3mico promisorio que motiva la continuaci\u00f3n de los programas de exploraci\u00f3n.<\/p>\n\t\t<\/div><!-- \/.fancy-box-header -->\n\t\t\n\t\t\t\t\n\t<\/div><!-- \/.fancy-box-contents -->\n\t\n\t\t\n<\/div><!-- \/.fancy-box fancy-box-classes --><style>@media (min-width: 992px) { .ld_spacer_6aea90eca4ab4{height:40px};}<\/style>\n<div class=\"ld-empty-space ld_spacer_6aea90eca4ab4\"><span class=\"liquid_empty_space_inner\"><\/span><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section><section data-bg-image=\"url\" class=\"vc_row wpb_row vc_row-fluid vc_custom_1762161554422 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-6aea90eca4dc8 vc_row-has-fill vc_row-has-bg vc_row-o-content-middle vc_row-flex\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 vc_col-md-8 liquid-column-6aea90eca5015\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\"><style>.ld_fancy_heading_6aea90eca5171 h3{font-size:50px;line-height:1.2em;font-weight:600;letter-spacing:-0.015em;color:rgb(255, 255, 255);}.ld_fancy_heading_6aea90eca5171 .lqd-highlight-inner{height:0.275em;bottom:0px;}<\/style><div class=\"ld-fancy-heading text-underline ld_fancy_heading_6aea90eca5171\">\n\t<h3 class=\"lqd-highlight-underline lqd-highlight-grow-left\" data-fittext=\"true\" data-fittext-options='{\"compressor\":0.55,\"maxFontSize\":\"50\",\"minFontSize\":\"35\"}' data-split-text=\"true\" data-custom-animations=\"true\" data-ca-options='{\"triggerHandler\":\"inview\",\"animationTarget\":\".lqd-chars .split-inner\",\"duration\":\"1200\",\"delay\":\"35\",\"easing\":\"easeOutQuint\",\"direction\":\"forward\",\"initValues\":{\"translateX\":2,\"translateY\":12,\"rotateZ\":6,\"opacity\":0},\"animations\":{\"translateX\":0,\"translateY\":0,\"rotateZ\":0,\"opacity\":1}}' data-split-options='{\"type\":\"chars, words\"}'><span class=\"ld-fh-txt\"> <span style=\"color: #ffffff\"><strong>Impulsado por nuestra pasi\u00f3n por la innovaci\u00f3n y compromiso con la excelencia.<\/strong><\/span><\/span><\/h3><\/div><\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-12 vc_col-md-offset-1 vc_col-md-3 text-left text-md-right liquid-column-6aea90eca5bde\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  data-custom-animations=\"true\" data-ca-options='{\"triggerHandler\":\"inview\",\"animationTarget\":\"all-childs\",\"duration\":\"1200\",\"delay\":\"150\",\"easing\":\"easeOutQuint\",\"direction\":\"forward\",\"initValues\":{\"translateY\":39,\"opacity\":0},\"animations\":{\"translateY\":0,\"opacity\":1}}' ><div class=\"wpb_wrapper-inner\"><div class=\"vc_empty_space\"   style=\"height: 25px\"><span class=\"vc_empty_space_inner\"><\/span><\/div><div class=\"vc_row wpb_row vc_inner vc_row-fluid liquid-row-shadowbox-6aea90eca5e52\"><div class=\"wpb_column vc_column_container vc_col-sm-12 text-left text-md-center liquid-column-6aea90eca5fec\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"  ><div class=\"wpb_wrapper-inner\"><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/section>\n<\/div>","protected":false},"excerpt":{"rendered":"Eficiencia y Excelencia en cada Etapa del Proceso Innovaci\u00f3n para el Futuro Minero Nos caracterizamos...","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-7868","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v26.3 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Potfolio Goliat - Goliat Minerals GROUP<\/title>\n<meta name=\"description\" content=\"Somos una empresa marroqu\u00ed especializada en la exploraci\u00f3n y desarrollo de proyectos mineros de gran potencial, con una visi\u00f3n orientada a la creaci\u00f3n de valor sostenible. 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