A rhyolite to dacite sequence of volcanism directly from the heated lower crust: Late Pleistocene to Holocene Numazawa volcano, NE Japan

Journal of Volcanology and Geothermal Research

Volumn 167, Issue 1-4, 2007, Pages 119-133

  Yamamoto, Takahiro ^a  

^a NATIONAL INSTITUTE OF ADVANCED INDUSTRIAL SCIENCE AND TECHNOLOGY AIST   (Japan)

Author keywords

geochemistry; Japan; Lower crustal melting; Numazawa volcano; Silicic volcanism

Indexed keywords

BASALT; CHEMICAL ANALYSIS; GEOCHEMISTRY; IGNEOUS ROCKS; SILICA; TEMPERATURE; VOLCANIC ROCKS; VOLCANOES;

DACITE SEQUENCE; LOWER CRUSTAL MELTING; SILICIC VOLCANISM;

GEOCHRONOLOGY;

DACITE; EJECTA; HOLOCENE; IGNEOUS GEOCHEMISTRY; ISOTOPIC COMPOSITION; MELTING; PLEISTOCENE; RHYOLITE; VOLCANISM;

ASIA; EURASIA; FAR EAST; FUKUSHIMA; HONSHU; JAPAN; NUMAZAWA VOLCANO; TOHOKU;

EID: 35448957193     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2007.05.011     Document Type: Article

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