{"id":7655,"date":"2025-01-13T20:10:46","date_gmt":"2025-01-13T20:10:46","guid":{"rendered":"https:\/\/quantecgeo.com\/?p=7655"},"modified":"2025-02-04T15:52:35","modified_gmt":"2025-02-04T15:52:35","slug":"spectacular-mt-results-under-red-lake","status":"publish","type":"post","link":"https:\/\/quantecgeo.com\/es\/spectacular-mt-results-under-red-lake\/","title":{"rendered":"Spectacular MT results under Red Lake"},"content":{"rendered":"<p>Newly released paper discusses MT applications and implications in the Red Lake Greenstone belt following Metal Earth initiative using SPARTAN MT .<\/p>\n<p><strong>Crustal conductivity footprint of the orogenic gold district in the <\/strong><br \/>\n<strong>Red Lake greenstone belt, western Superior craton, Canada<\/strong><br \/>\nAdemola Q. Adetunji1, Gaetan Launay1, Ian J. Ferguson2, Jack M. Simmons1, Chong Ma1, John Ayer1 and Bruno Lafrance1<br \/>\n1Mineral Exploration Research Centre (MERC), Harquail School of Earth Sciences, Laurentian University, Sudbury, ON P3E2C6, Canada<br \/>\n2Department of Earth Sciences, University of Manitoba, Winnipeg, MB R3T2N2, Canada<\/p>\n<p><strong>ABSTRACT<\/strong><br \/>\nA magnetotelluric (MT) study across the Red Lake greenstone belt of the western Superior craton, Canada, images a 50-km-long north-dipping conductor (&lt;20 \u03a9\u00b7m) at 20\u201325 km<br \/>\ndepth and subvertical conductors spatially correlated with crustal-scale shear zones and<br \/>\nlarge orogenic gold deposits. The conductors are interpreted to be the conductivity signature<br \/>\nof the deep crustal source of the auriferous fluids and pathways of the orogenic gold system. The geophysical results, supported by existing geochemical and fluid inclusion studies,<br \/>\nsuggest that the Au- and CO2-rich fluids responsible for gold mineralization were released<br \/>\nby devolatilization of supracrustal rocks underthrust to mid- to lower-crustal levels during<br \/>\nsubduction. This MT study links shallow gold mineralization to a deep crustal source region,<br \/>\ndemonstrating the connection between a crustal suture zone and the formation of orogenic<br \/>\ngold deposits in an Archean greenstone belt.<\/p>\n<p>&nbsp;<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-7657\" src=\"https:\/\/quantecgeo.com\/wp-content\/uploads\/2023\/03\/fig-from-paper.jpg\" alt=\"\" width=\"740\" height=\"841\" srcset=\"https:\/\/quantecgeo.com\/wp-content\/uploads\/2023\/03\/fig-from-paper.jpg 740w, https:\/\/quantecgeo.com\/wp-content\/uploads\/2023\/03\/fig-from-paper-264x300.jpg 264w, https:\/\/quantecgeo.com\/wp-content\/uploads\/2023\/03\/fig-from-paper-620x705.jpg 620w\" sizes=\"auto, (max-width: 740px) 100vw, 740px\" \/><\/p>","protected":false},"excerpt":{"rendered":"<p>Newly released paper discusses MT applications and implications in the Red Lake Greenstone belt following Metal Earth initiative using SPARTAN MT . Crustal conductivity footprint of the orogenic gold district in the Red Lake greenstone belt, western Superior craton, Canada Ademola Q. Adetunji1, Gaetan Launay1, Ian J. Ferguson2, Jack M. Simmons1, Chong Ma1, John Ayer1 [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":7656,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3],"tags":[],"class_list":["post-7655","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-client-press"],"_links":{"self":[{"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/posts\/7655","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/comments?post=7655"}],"version-history":[{"count":0,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/posts\/7655\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/media\/7656"}],"wp:attachment":[{"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/media?parent=7655"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/categories?post=7655"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/tags?post=7655"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}