Subvolcanic gabbro–porphyrite and intrusive diorite, and sulfide mineralization of the Dzhusa volcanogenic massive sulfide deposit (Southern Urals)
- 作者: Yartsev E.I.1,2, Eremin N.I.1,2, Vikentyev I.V.2,3
-
隶属关系:
- Lomonosov Moscow State University
- Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry
- RUDN University
- 期: 卷 476, 编号 1 (2017)
- 页面: 1007-1009
- 栏目: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/190709
- DOI: https://doi.org/10.1134/S1028334X17090215
- ID: 190709
如何引用文章
详细
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.
作者简介
E. Yartsev
Lomonosov Moscow State University; Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry
编辑信件的主要联系方式.
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
补充文件
