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Low-Temperature Acidic Melts of Bazman Volcano (Iran)


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

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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