Petrological and chronological study of primitive high-Mg andesite from monogenetic volcanoes in the fore-arc region of northern Kamchatka Peninsula

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dc.contributor.author Nishizawa Tatsuji
dc.contributor.author Nakamura Hitomi
dc.contributor.author Churikova Tatiana
dc.contributor.author Gordeychik Boris
dc.contributor.author Ishizuka Osamu
dc.contributor.author Iwamori Hikaru
dc.date.accessioned 2019-09-03T05:55:38Z
dc.date.available 2019-09-03T05:55:38Z
dc.date.issued 2014-09-22
dc.identifier http://repo.kscnet.ru/3043/
dc.identifier http://repo.kscnet.ru/3043/1/Nishizawa_2014 JKASP.pdf
dc.identifier http://hkdrcep.sci.hokudai.ac.jp/map/jkasp2014/pdf/J32.pdf
dc.identifier.citation Nishizawa Tatsuji, Nakamura Hitomi, Churikova Tatiana, Gordeychik Boris, Ishizuka Osamu, Iwamori Hikaru (2014) Petrological and chronological study of primitive high-Mg andesite from monogenetic volcanoes in the fore-arc region of northern Kamchatka Peninsula // 8th Biennial Workshop on Japan-Kamchatka-Alaska Subduction Processes. Finding clues for science and disaster mitigation from international collaboration (JKASP-2014), 22-26 September 2014, Sapporo, Japan. Sapporo, Japan: Hokkaido University. pp. 1-2.
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/5836
dc.description.abstract Primitive high-Mg andesites (HMA) exhibit low FeO*/MgO (FeO*, total iron) and high Mg# (=100×Mg/(Mg+Fe)), and are thought to be generated by hydrous mantle melting (Kushiro, 1969). HMA, including sanukitoids of the Setouchi volcanic belt, have been recognized in many orogenic belts of various ages, and in several cases, constitute a part of ophiolite (Tatsumi, 2003). Therefore, occurrence of HMA in northern Kamchatka may have important implications on the tectonic setting of the peninsula and/or the melting condition underneath.
dc.language.iso en
dc.publisher Hokkaido University
dc.subject 38.33.17 Геохимия природных процессов
dc.title Petrological and chronological study of primitive high-Mg andesite from monogenetic volcanoes in the fore-arc region of northern Kamchatka Peninsula
dc.type Конференционный материал


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