Subvolcanic gabbro–porphyrite and intrusive diorite, and sulfide mineralization of the Dzhusa volcanogenic massive sulfide deposit (Southern Urals)


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Two sequentially formed groups of dikes in the gabbro–porphyrite complex have been distinguished, the ages of which are early Eifelian (early dikes) and early Givetian (late dikes). We have estimated the temperature impact of ore contact metamorphism, which is related to dikes of the Lower Carboniferous Magnitogorsk intrusive complex. A hidden zonality of microimpurities in the ore-forming minerals has been established for the first time by the LA-ICP-MS method. The ore formation age has been determined as early Eifelian–early Givetian.

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E. Yartsev

Lomonosov Moscow State University; Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry

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Email: evgenyrtsev@mail.ru
俄罗斯联邦, Moscow; Moscow, 119017

N. Eremin

Lomonosov Moscow State University; Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry

Email: evgenyrtsev@mail.ru
俄罗斯联邦, Moscow; Moscow, 119017

I. Vikentyev

Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry; RUDN University

Email: evgenyrtsev@mail.ru
俄罗斯联邦, Moscow, 119017; Moscow

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