Geochemical Features of Cupriferous Sandstones in the Orenburg Area of the Ural Region
- Autores: Volkov A.1, Novikov I.1, Razumovskiy A.2, Murashov K.1, Sidorova N.1, Sidorov A.1
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Afiliações:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Geological Institute
- Edição: Volume 479, Nº 1 (2018)
- Páginas: 393-396
- Seção: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/192577
- DOI: https://doi.org/10.1134/S1028334X18030339
- ID: 192577
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Resumo
The new geochemical data obtained of cupriferous sandstones of the Orenburg area of the Ural region show that the Permian host stratum could have served as the source of rare-earth elements and other microelements for the ore-forming fluids. They confirm the possibility of using a convection model to explain the genesis of the copper ores studied. This model indicates the likely multistage development of mineralization to significant depths, like in the Manto deposits in Chili. Consequently, the Permian cupriferous sandstones of the southwestern area of the Ural region can be considered a very promising source of raw material for the development of copper industry in the area.
Sobre autores
A. Volkov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Autor responsável pela correspondência
Email: tma2105@mail.ru
Rússia, Moscow, 119017
I. Novikov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tma2105@mail.ru
Rússia, Moscow, 119017
A. Razumovskiy
Geological Institute
Email: tma2105@mail.ru
Rússia, Moscow, 119017
K. Murashov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tma2105@mail.ru
Rússia, Moscow, 119017
N. Sidorova
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tma2105@mail.ru
Rússia, Moscow, 119017
A. Sidorov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tma2105@mail.ru
Rússia, Moscow, 119017