Origin of silicic magmas and the compositional gap at Sumisu submarine caldera, Izu-Bonin arc, Japan

Journal of Volcanology and Geothermal Research

Volumn 156, Issue 3-4, 2006, Pages 187-216

  Shukuno, H ^a   Tamura, Y ^a   Tani, K ^a   Chang, Q ^a   Suzuki, T ^a   Fiske, R S ^b  

^a JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^b SMITHSONIAN INSTITUTION   (United States)

Author keywords

andesite protolith; caldera; dacite; oceanic arc; partial melting; remobilization; rhyolite

Indexed keywords

CRYSTALLIZATION; DEHYDRATION; INCLUSIONS; MELTING; SUBMARINE GEOLOGY; VOLCANIC ROCKS; VOLCANOES;

ANDESITE PROTOLITH; PARTIAL MELTING; REMOBILIZATION; SILICIC MAGMAS;

SEISMOLOGY;

ANDESITE; BASALT; CALDERA; DACITE; MAGMA; PARTIAL MELTING; PROTOLITH; REMOBILIZATION; RHYOLITE; VOLCANO;

ASIA; EURASIA; FAR EAST; IZU-BONIN ARC; JAPAN; PACIFIC OCEAN;

EID: 33747328885     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2006.03.018     Document Type: Article

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