Мақаланы E-mail арқылы жіберу Low-Temperature Acidic Melts of Bazman Volcano (Iran)
- Авторлар: 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
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Мекемелер:
- 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
- Шығарылым: Том 485, № 2 (2019)
- Беттер: 422-425
- Бөлім: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/194827
- DOI: https://doi.org/10.1134/S1028334X19040147
- ID: 194827
Дәйексөз келтіру
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Рұқсат берілді
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Аннотация
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.
Авторлар туралы
V. Prokofiev
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences
Хат алмасуға жауапты Автор.
Email: vpr2004@rambler.ru
Ресей, Moscow, 119017
V. Naumov
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
Хат алмасуға жауапты Автор.
Email: naumov@geokhi.ru
Ресей, Moscow, 119991
A. Roman’ko
Geological Institute, Russian Academy of Sciences
Email: naumov@geokhi.ru
Ресей, Moscow, 119017
A. Balashova
Institute of Geochemistry and Petrology, Swiss Federal Institute of Technology (ETH Zurich)
Email: naumov@geokhi.ru
Швейцария, Zurich
P. Plechov
Moscow State University
Email: naumov@geokhi.ru
Ресей, Moscow, 119234
N. Imamverdiyev
Baku State University
Email: naumov@geokhi.ru
Әзірбайжан, Baku
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