Low-Temperature Acidic Melts of Bazman Volcano (Iran)
- Autores: Prokofiev V.Y.1, Naumov V.B.2, Roman’ko A.E.3, Balashova A.L.4, Plechov P.Y.5, Imamverdiyev N.A.6
-
Afiliações:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences
- Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
- Geological Institute, Russian Academy of Sciences
- Institute of Geochemistry and Petrology, Swiss Federal Institute of Technology (ETH Zurich)
- Moscow State University
- Baku State University
- Edição: Volume 485, Nº 2 (2019)
- Páginas: 422-425
- Seção: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/194827
- DOI: https://doi.org/10.1134/S1028334X19040147
- ID: 194827
Citar
Resumo
The inclusions of a silicate melt were investigated in quartz insets of the extrusive rhyolite collected at Bazman Cenozoic volcano (Iran) and associated with the process of recent subduction. Low temperatures of the silicate melt along with high concentrations of water in the melt are ascertained. The microelemental composition of the melt showed a similarity to acidic melts of island–arc formations.
Sobre autores
V. Prokofiev
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences
Autor responsável pela correspondência
Email: vpr2004@rambler.ru
Rússia, Moscow, 119017
V. Naumov
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
Autor responsável pela correspondência
Email: naumov@geokhi.ru
Rússia, Moscow, 119991
A. Roman’ko
Geological Institute, Russian Academy of Sciences
Email: naumov@geokhi.ru
Rússia, Moscow, 119017
A. Balashova
Institute of Geochemistry and Petrology, Swiss Federal Institute of Technology (ETH Zurich)
Email: naumov@geokhi.ru
Suíça, Zurich
P. Plechov
Moscow State University
Email: naumov@geokhi.ru
Rússia, Moscow, 119234
N. Imamverdiyev
Baku State University
Email: naumov@geokhi.ru
Azerbaijão, Baku
Arquivos suplementares
