Low-Temperature Acidic Melts of Bazman Volcano (Iran)


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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.

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V. Prokofiev

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences

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Email: vpr2004@rambler.ru
俄罗斯联邦, Moscow, 119017

V. Naumov

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences

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Email: naumov@geokhi.ru
俄罗斯联邦, Moscow, 119991

A. Roman’ko

Geological Institute, Russian Academy of Sciences

Email: naumov@geokhi.ru
俄罗斯联邦, Moscow, 119017

A. Balashova

Institute of Geochemistry and Petrology, Swiss Federal Institute of Technology (ETH Zurich)

Email: naumov@geokhi.ru
瑞士, Zurich

P. Plechov

Moscow State University

Email: naumov@geokhi.ru
俄罗斯联邦, Moscow, 119234

N. Imamverdiyev

Baku State University

Email: naumov@geokhi.ru
阿塞拜疆, Baku

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