{"id":60,"date":"2015-09-30T19:09:54","date_gmt":"2015-09-30T19:09:54","guid":{"rendered":"http:\/\/magnumgoldcorp.com\/?page_id=60"},"modified":"2015-10-02T02:24:12","modified_gmt":"2015-10-02T02:24:12","slug":"geology","status":"publish","type":"page","link":"http:\/\/magnumgoldcorp.com\/index.php\/lh-gold-project\/geology\/","title":{"rendered":"Geology"},"content":{"rendered":"<p>The LH Property lies within a Triassic\/Jurassic sedimentary\/volcanic roof pendant lying with granodiorite intrusives of the Nelson Batholith. The sedimentary rocks consist of the Slocan Group of<\/p>\n<figure id=\"attachment_144\" aria-describedby=\"caption-attachment-144\" style=\"width: 300px\" class=\"wp-caption alignright\"><a href=\"http:\/\/magnumgoldcorp.com\/wp-content\/uploads\/2015\/09\/Geology.png\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-144 size-medium\" src=\"http:\/\/magnumgoldcorp.com\/wp-content\/uploads\/2015\/09\/Geology-300x174.png\" alt=\"LH Property Geology\" width=\"300\" height=\"174\" srcset=\"http:\/\/magnumgoldcorp.com\/wp-content\/uploads\/2015\/09\/Geology-300x174.png 300w, http:\/\/magnumgoldcorp.com\/wp-content\/uploads\/2015\/09\/Geology-1024x593.png 1024w, http:\/\/magnumgoldcorp.com\/wp-content\/uploads\/2015\/09\/Geology.png 1500w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><figcaption id=\"caption-attachment-144\" class=\"wp-caption-text\">LH Property Geology<\/figcaption><\/figure>\n<p>sediments which consist of a flysch sequence of immature sandstones, siltstones and shales. The Slocan sediments conformably underlie Rossland Volcanics which consist of a chaotic sequence of intermediate tuff, lapilli tuff and agglomerate.<\/p>\n<p>Detailed mapping revealed a series of alteration zones across the large package of pyroclastics forming the ridge. From the east side where the tuff and agglomerate is relatively unaltered, alteration increases gradually to the west, distinguished by an increase in biotite hornfels alteration, chlorite and hornblende alteration with local potassic and sericite alteration. On the west side, the intensity of alteration increases to form zones of well-developed biotite hornfels and pyroxene and epidote calc- silicates in the southwest corner of the ridge. In addition, pervasive silicification throughout a wide central zone forms the steep ridge running approximately north- south. This zone is important as it is the primary host to sulphides associated with anomalous gold mineralization.<\/p>\n<p>Gold mineralization occurs in structurally controlled mesothermal quartz veins along with pyrite, arsenopyrite, and chalcopyrite. Gold also occurs in a stockwork zone of silicified and hornfelsed volcanics. This mineralization is associated primarily with pyrrhotite and arsenopyrite, and minor chalcopyrite.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>The LH Property lies within a Triassic\/Jurassic sedimentary\/volcanic roof pendant lying with granodiorite intrusives of the Nelson Batholith. The sedimentary rocks consist of the Slocan Group of sediments which consist of a flysch sequence of immature sandstones, siltstones and shales. The Slocan sediments conformably underlie Rossland Volcanics which consist of [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":29,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-right-sidebar.php","meta":{"footnotes":""},"class_list":["post-60","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Geology - Magnum Goldcorp Inc.<\/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:\/\/magnumgoldcorp.com\/index.php\/lh-gold-project\/geology\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Geology - Magnum Goldcorp Inc.\" \/>\n<meta property=\"og:description\" content=\"The LH Property lies within a Triassic\/Jurassic sedimentary\/volcanic roof pendant lying with granodiorite intrusives of the Nelson Batholith. The sedimentary rocks consist of the Slocan Group of sediments which consist of a flysch sequence of immature sandstones, siltstones and shales. The Slocan sediments conformably underlie Rossland Volcanics which consist of [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/magnumgoldcorp.com\/index.php\/lh-gold-project\/geology\/\" \/>\n<meta property=\"og:site_name\" content=\"Magnum Goldcorp Inc.\" \/>\n<meta property=\"article:modified_time\" content=\"2015-10-02T02:24:12+00:00\" \/>\n<meta property=\"og:image\" content=\"http:\/\/magnumgoldcorp.com\/wp-content\/uploads\/2015\/09\/Geology-300x174.png\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"1 minute\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/magnumgoldcorp.com\\\/index.php\\\/lh-gold-project\\\/geology\\\/\",\"url\":\"https:\\\/\\\/magnumgoldcorp.com\\\/index.php\\\/lh-gold-project\\\/geology\\\/\",\"name\":\"Geology - Magnum Goldcorp Inc.\",\"isPartOf\":{\"@id\":\"http:\\\/\\\/magnumgoldcorp.com\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\\\/\\\/magnumgoldcorp.com\\\/index.php\\\/lh-gold-project\\\/geology\\\/#primaryimage\"},\"image\":{\"@id\":\"https:\\\/\\\/magnumgoldcorp.com\\\/index.php\\\/lh-gold-project\\\/geology\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/magnumgoldcorp.com\\\/wp-content\\\/uploads\\\/2015\\\/09\\\/Geology-300x174.png\",\"datePublished\":\"2015-09-30T19:09:54+00:00\",\"dateModified\":\"2015-10-02T02:24:12+00:00\",\"breadcrumb\":{\"@id\":\"https:\\\/\\\/magnumgoldcorp.com\\\/index.php\\\/lh-gold-project\\\/geology\\\/#breadcrumb\"},\"inLanguage\":\"en\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\\\/\\\/magnumgoldcorp.com\\\/index.php\\\/lh-gold-project\\\/geology\\\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en\",\"@id\":\"https:\\\/\\\/magnumgoldcorp.com\\\/index.php\\\/lh-gold-project\\\/geology\\\/#primaryimage\",\"url\":\"http:\\\/\\\/magnumgoldcorp.com\\\/wp-content\\\/uploads\\\/2015\\\/09\\\/Geology.png\",\"contentUrl\":\"http:\\\/\\\/magnumgoldcorp.com\\\/wp-content\\\/uploads\\\/2015\\\/09\\\/Geology.png\",\"width\":1500,\"height\":869,\"caption\":\"LH Property Geology\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\\\/\\\/magnumgoldcorp.com\\\/index.php\\\/lh-gold-project\\\/geology\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"http:\\\/\\\/magnumgoldcorp.com\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"LH Gold Project\",\"item\":\"https:\\\/\\\/magnumgoldcorp.com\\\/index.php\\\/lh-gold-project\\\/\"},{\"@type\":\"ListItem\",\"position\":3,\"name\":\"Geology\"}]},{\"@type\":\"WebSite\",\"@id\":\"http:\\\/\\\/magnumgoldcorp.com\\\/#website\",\"url\":\"http:\\\/\\\/magnumgoldcorp.com\\\/\",\"name\":\"Magnum Goldcorp Inc.\",\"description\":\"TSX.V: MGI\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"http:\\\/\\\/magnumgoldcorp.com\\\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Geology - Magnum Goldcorp Inc.","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/magnumgoldcorp.com\/index.php\/lh-gold-project\/geology\/","og_locale":"en_US","og_type":"article","og_title":"Geology - Magnum Goldcorp Inc.","og_description":"The LH Property lies within a Triassic\/Jurassic sedimentary\/volcanic roof pendant lying with granodiorite intrusives of the Nelson Batholith. The sedimentary rocks consist of the Slocan Group of sediments which consist of a flysch sequence of immature sandstones, siltstones and shales. 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