{"id":3849,"date":"2019-11-05T18:28:23","date_gmt":"2019-11-05T18:28:23","guid":{"rendered":"https:\/\/www.gsnv.org\/shop\/porphyry-related-deposits-of-nevada\/"},"modified":"2020-02-24T18:20:54","modified_gmt":"2020-02-24T18:20:54","slug":"porphyry-related-deposits-of-nevada","status":"publish","type":"product","link":"https:\/\/www.gsnv.org\/shop\/porphyry-related-deposits-of-nevada\/","title":{"rendered":"Porphyry-Related Deposits of Nevada"},"content":{"rendered":"","protected":false},"excerpt":{"rendered":"

Welcome to the Geological Society of Nevada\u2019s 2015 Symposium Field Trip, Porphyry-Related
\nDeposits of Nevada. When explorationists and miners convene in Nevada, gold deposits and
\nproduction dominate conversations, but copper should not be considered a deserted step-child. For
\nexample, 19th century prospectors began mining high-grade copper from skarn deposits in the
\nYerington district shortly after discovery of the bonanza Au-Ag discoveries at the Comstock Lode.
\nCopper mining began in earnest during the early 1900\u2019s with the advent of and financial benefit
\nfrom bulk-tonnage open pit mining in the Ruth mine at Ely, now part of KGHM\u2019s Robinson copper
\nmine, which operated nearly continuously over a 100+ year history. Major copper production
\ncontinued during the mid-1950\u2019s when the Anaconda Company commissioned their Yerington mine
\nin Lyon County followed by, in late 1970\u2019s, another porphyry-hosted deposit, Anaconda\u2019s Hall mine
\nin Nye County, albeit dominated by molybdenum with minor copper. Modern porphyry exploration
\nincludes General Moly\u2019s Mount Hope property in Eureka County, representing another
\nmolybdenum-dominated porphyry deposit.
\nOur field trip will take us to the Robinson mine at Ely and on to the Yerington district, sharing
\nsimilarities of porphyry-derived copper mineralization dismembered by Tertiary extensional faulting.
\nBoth districts include skarn deposits (current mining at Robinson, planned 2016 mining in the
\nYerington district) hosted in upper Paleozoic and Mesozoic carbonates and calcareous siltstones,
\nrespectively. Copper mineralization at Robinson derives from mid-Cretaceous monzonite \/ quartz
\nmonzonite intruded into an upper Paleozoic section that is also credited with gold production from
\ndeposits peripheral to the copper pits. The Yerington district is currently being explored by three
\ncompanies with mining planned by Nevada Copper in 2016 on copper-magnetite skarn
\nmineralization hosted in mid-Triassic \/ early Jurassic carbonates and calcareous siltstones. Copper is
\nhosted mid-Jurassic granodiorite and quartz monzonite and, significantly, in related dikes which host
\nmajor copper mineralization at Entr\u00e9e Gold\u2019s Ann Mason deposit and at Singatse Peak Services\u2019
\nBear sulfide deposit, MacArthur oxide \u2013 sulfide copper deposit, and unmined sulfide mineralization
\nremaining in the Yerington pit.
\nThe three-day field trip will depart Reno on Thursday, May 21, arriving in Ely that evening for
\ndinner and a presentation of Robinson mine geology by KGHM geologists who will tour us through
\nseveral of the pits at Robinson on Friday morning. Departing Friday afternoon from Ely will take us
\nback along US Highway 50 to Fernley, then south to overnight in Yerington. Friday\u2019s dinner
\ndiscussion in Yerington will feature Singatse Peak Services\u2019 (SPS) geologists describing the Bear,
\nYerington mine, and MacArthur deposits. Saturday morning will begin with visits to SPS\u2019s Yerington
\nmine, Bear overlook, and MacArthur 4680 bench which will also include Entr\u00e9e Gold geologists
\npresenting a core shack examination and discussion of their Ann Mason deposit. The Yerington tour
\nwill conclude with an overview of Nevada Copper\u2019s Pumpkin Hollow deposit at the East \/ E-2<\/p>\n","protected":false},"featured_media":4786,"comment_status":"closed","ping_status":"closed","template":"","meta":{"pmpro_default_level":""},"product_cat":[811],"product_tag":[],"_links":{"self":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product\/3849"}],"collection":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product"}],"about":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/types\/product"}],"replies":[{"embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/comments?post=3849"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/media\/4786"}],"wp:attachment":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/media?parent=3849"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product_cat?post=3849"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product_tag?post=3849"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}