{"id":444,"date":"2021-09-28T11:57:46","date_gmt":"2021-09-28T03:57:46","guid":{"rendered":"https:\/\/www.xanadumines.com\/?page_id=444"},"modified":"2021-09-28T15:37:07","modified_gmt":"2021-09-28T07:37:07","slug":"geology-and-mineralisation","status":"publish","type":"page","link":"https:\/\/www.xanadumines.com\/kharmagtai\/geology-and-mineralisation\/","title":{"rendered":"Geology &#038; Mineralisation"},"content":{"rendered":"\n<div class=\"wp-block-genesis-blocks-gb-container alignfull hero gb-block-container\"><div class=\"gb-container-inside\"><div class=\"gb-container-image-wrap\"><img decoding=\"async\" class=\"gb-container-image has-background-dim-100 has-background-dim\" src=\"https:\/\/www.xanadumines.com\/wp-content\/uploads\/project-hero-bg.jpg\" alt=\"\"\/><\/div><div class=\"gb-container-content\">\n<div style=\"height:120px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p class=\"has-text-align-center has-white-color has-text-color has-huge-font-size\"><strong>Projects<\/strong><\/p>\n\n\n\n<hr class=\"wp-block-separator has-text-color has-background has-theme-primary-background-color has-theme-primary-color\"\/>\n\n\n\n<div style=\"height:170px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-container alignfull breadcrumb-container gb-block-container\"><div class=\"gb-container-inside\"><div class=\"gb-container-content\"><div class=\"yoast-breadcrumbs\"><span><span><a href=\"https:\/\/www.xanadumines.com\/\">Home<\/a><\/span> \u00bb <span><a href=\"https:\/\/www.xanadumines.com\/kharmagtai\/\">Kharmagtai<\/a><\/span> \u00bb <span class=\"breadcrumb_last\" aria-current=\"page\">Geology &#038; Mineralisation<\/span><\/span><\/div><\/div><\/div><\/div>\n\n\n\n<div style=\"height:100px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-columns content-columns gb-layout-columns-2 gb-2-col-wideright alignfull\"><div class=\"gb-layout-column-wrap gb-block-layout-column-gap-8 gb-is-responsive-column\">\n<div class=\"wp-block-genesis-blocks-gb-column menu-column gb-block-layout-column\"><div class=\"gb-block-layout-column-inner gb-has-custom-background-color\" style=\"padding:20px;background-color:#f6f7fc\"><div class=\"sidebar-menu-container\"><ul id=\"menu-projects-menu\" class=\"menu\"><li id=\"menu-item-435\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-435\"><a href=\"https:\/\/www.xanadumines.com\/project-overview\/\">Project Overview<\/a><\/li>\n<li id=\"menu-item-440\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-has-children menu-item-440\"><a href=\"https:\/\/www.xanadumines.com\/kharmagtai\/\">Kharmagtai<\/a>\n<ul class=\"sub-menu\">\n\t<li id=\"menu-item-1180\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-1180\"><a href=\"https:\/\/www.xanadumines.com\/kharmagtai\/strategic-partnership-with-zijin-mining-group\/\">Strategic Partnership with Zijin Mining Group<\/a><\/li>\n\t<li id=\"menu-item-496\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-496\"><a href=\"https:\/\/www.xanadumines.com\/kharmagtai\/geology-and-mineralisation\/\">Geology &#038; Mineralisation<\/a><\/li>\n\t<li id=\"menu-item-495\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-495\"><a href=\"https:\/\/www.xanadumines.com\/kharmagtai\/geophysics\/\">Geophysics<\/a><\/li>\n\t<li id=\"menu-item-494\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-494\"><a href=\"https:\/\/www.xanadumines.com\/kharmagtai\/resources\/\">Resources<\/a><\/li>\n\t<li id=\"menu-item-1092\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-1092\"><a href=\"https:\/\/www.xanadumines.com\/kharmagtai\/pre-feasibility-study\/\">Pre-Feasibility Study (PFS)<\/a><\/li>\n\t<li id=\"menu-item-493\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-493\"><a href=\"https:\/\/www.xanadumines.com\/kharmagtai\/undercover-initiative\/\">Undercover Initiative<\/a><\/li>\n\t<li id=\"menu-item-492\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-492\"><a href=\"https:\/\/www.xanadumines.com\/kharmagtai\/zaraa-discovery\/\">Zaraa Discovery<\/a><\/li>\n<\/ul>\n<\/li>\n<li id=\"menu-item-500\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-500\"><a href=\"https:\/\/www.xanadumines.com\/red-mountain\/\">Red Mountain<\/a><\/li>\n<\/ul><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column\"><div class=\"gb-block-layout-column-inner\">\n<h1 class=\"has-huge-font-size wp-block-heading\"><strong><strong><strong><strong><strong><strong><strong><strong><strong>Geology &amp; Mineralisation<\/strong><\/strong><\/strong><\/strong><\/strong><\/strong><\/strong><\/strong><\/strong><\/h1>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h2 class=\"has-normal-font-size wp-block-heading\">Geology<\/h2>\n\n\n\n<p>Kharmagtai consists of multiple co-genetic gold-rich porphyry copper centres and tourmaline breccia pipes occurring within the Carboniferous Kharmagtai Igneous Complex. The Kharmagtai Igneous Complex consists of a series of intrusive bodies ranging between diorite through monzodiorite, quartz-monzodiorite to monzonite and granodiorite compositions. This cluster of intrusives is interpreted to be formed from a very large fractionating magma chamber at depth. The extents of this magma chamber can be seen in the recent gravity survey (see geophysics section).<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1920\" height=\"1362\" src=\"https:\/\/www.xanadumines.com\/wp-content\/uploads\/Kharmagtai-License-Map-Geology.jpg\" alt=\"\" class=\"wp-image-447\" srcset=\"https:\/\/www.xanadumines.com\/wp-content\/uploads\/Kharmagtai-License-Map-Geology.jpg 1920w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Kharmagtai-License-Map-Geology-300x213.jpg 300w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Kharmagtai-License-Map-Geology-1024x726.jpg 1024w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Kharmagtai-License-Map-Geology-768x545.jpg 768w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Kharmagtai-License-Map-Geology-1536x1090.jpg 1536w\" sizes=\"(max-width: 1920px) 100vw, 1920px\" \/><figcaption>Kharmagtai License Map &amp; Geology<\/figcaption><\/figure>\n\n\n\n<h2 class=\"has-normal-font-size wp-block-heading\">Mineralisation<\/h2>\n\n\n\n<p>There are three styles of mineralisation at Kharmagtai; porphyry style stock work Cu-Au mineralisation, tourmaline breccia style Cu-Au mineralisation and epithermal gold associated with carbonate base metal veins.<\/p>\n\n\n\n<p><strong>Porphyry mineralisation\u00a0<\/strong>at Kharmagtai consists of chalcopyrite as disseminations and within high-density stock work quartz-sulphide veins. This is a very common style of Cu-Au mineralisation and forms the basis of the largest copper deposits in the world. At Kharmagtai porphyry mineralisation represents the larger portion of the defined resources (see resources section).<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"2400\" height=\"1210\" src=\"https:\/\/www.xanadumines.com\/wp-content\/uploads\/Porphyry-stock-work-mineralisation-from-KHDDH383.jpg\" alt=\"\" class=\"wp-image-448\" srcset=\"https:\/\/www.xanadumines.com\/wp-content\/uploads\/Porphyry-stock-work-mineralisation-from-KHDDH383.jpg 2400w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Porphyry-stock-work-mineralisation-from-KHDDH383-300x151.jpg 300w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Porphyry-stock-work-mineralisation-from-KHDDH383-1024x516.jpg 1024w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Porphyry-stock-work-mineralisation-from-KHDDH383-768x387.jpg 768w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Porphyry-stock-work-mineralisation-from-KHDDH383-1536x774.jpg 1536w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Porphyry-stock-work-mineralisation-from-KHDDH383-2048x1033.jpg 2048w\" sizes=\"(max-width: 2400px) 100vw, 2400px\" \/><figcaption>Porphyry stock work mineralisation from KHDDH383 @ 114m &#8211; 2m @ 4.37g\/t Au and 1.62% Cu<\/figcaption><\/figure>\n\n\n\n<p><strong>Tourmaline Breccia<\/strong>\u00a0mineralisation at Kharmagtai consists of chalcopyrite-tourmaline- pyrite as infill to hydrothermal breccia\u2019s that overprint the younger porphyry style mineralisation. \u00a0The tourmaline breccia Cu-Au mineralisation at Kharmagtai is a new style of mineralisation for Mongolia, although elsewhere in the world this type of mineralisation represents a significant source of copper and is currently being mined at Anglo American\u2019s\u00a0 Los Sulfatos deposit in Chile. At Kharmagtai, tourmaline breccia mineralisation was discovered by Xanadu beneath the porphyry stockwork zones at Stockwork Hill in 2015.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"2400\" height=\"1350\" src=\"https:\/\/www.xanadumines.com\/wp-content\/uploads\/Tourmaline-breccia-style-mineralisation-from-KHDDH344.jpg\" alt=\"\" class=\"wp-image-449\" srcset=\"https:\/\/www.xanadumines.com\/wp-content\/uploads\/Tourmaline-breccia-style-mineralisation-from-KHDDH344.jpg 2400w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Tourmaline-breccia-style-mineralisation-from-KHDDH344-300x169.jpg 300w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Tourmaline-breccia-style-mineralisation-from-KHDDH344-1024x576.jpg 1024w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Tourmaline-breccia-style-mineralisation-from-KHDDH344-768x432.jpg 768w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Tourmaline-breccia-style-mineralisation-from-KHDDH344-1536x864.jpg 1536w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Tourmaline-breccia-style-mineralisation-from-KHDDH344-2048x1152.jpg 2048w\" sizes=\"(max-width: 2400px) 100vw, 2400px\" \/><figcaption>Tourmaline breccia style mineralisation from KHDDH344 @ 392m &#8211; 2m @ 0.59g\/t Au and 0.63% Cu<\/figcaption><\/figure>\n\n\n\n<p>Epithermal gold mineralisation at Kharmagtai at hosted by carbonate-pyrite-chalcopyrite-sphalerite-galena veins controlled by late NW trending faults. Gold grades within these veins can range up to 190g\/t Au. This style of mineralisation has not been a focus for exploration at Kharmagtai, although significant potential exists for a high-grade gold resource from epithermal veins on the lease.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"2400\" height=\"1350\" src=\"https:\/\/www.xanadumines.com\/wp-content\/uploads\/Epithermal-style-mineralisation-from-KHRC257.jpg\" alt=\"\" class=\"wp-image-450\" srcset=\"https:\/\/www.xanadumines.com\/wp-content\/uploads\/Epithermal-style-mineralisation-from-KHRC257.jpg 2400w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Epithermal-style-mineralisation-from-KHRC257-300x169.jpg 300w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Epithermal-style-mineralisation-from-KHRC257-1024x576.jpg 1024w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Epithermal-style-mineralisation-from-KHRC257-768x432.jpg 768w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Epithermal-style-mineralisation-from-KHRC257-1536x864.jpg 1536w, https:\/\/www.xanadumines.com\/wp-content\/uploads\/Epithermal-style-mineralisation-from-KHRC257-2048x1152.jpg 2048w\" sizes=\"(max-width: 2400px) 100vw, 2400px\" \/><figcaption>Epithermal style mineralisation from KHRC257 @ 203m &#8211; 0.3m @ 42.7g\/t Au, 5.38% Cu, 1.52% Zn<\/figcaption><\/figure>\n<\/div><\/div>\n<\/div><\/div>\n\n\n\n<div style=\"height:100px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":2,"featured_media":0,"parent":437,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-templates\/blocks.php","meta":{"_acf_changed":false,"_genesis_hide_title":false,"_genesis_hide_breadcrumbs":false,"_genesis_hide_singular_image":false,"_genesis_hide_footer_widgets":false,"_genesis_custom_body_class":"","_genesis_custom_post_class":"","_genesis_layout":"","footnotes":""},"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v22.5 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Geology &amp; Mineralisation &#8226; Xanadu Mines<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.xanadumines.com\/kharmagtai\/geology-and-mineralisation\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Geology &amp; 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