Wet and dry basalt magma evolution at Torishima volcano, Izu-Bonin arc, Japan: The possible role of phengite in the downgoing slab

Journal of Petrology

Volumn 48, Issue 10, 2007, Pages 1999-2031

  Tamura, Y ^a   Tani, K ^a   Chang, Q ^a   Shukuno, H ^a   Kawabata, H ^a   Ishizuka, O ^b   Fiske, R S ^c  

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

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

^c SMITHSONIAN INSTITUTION   (United States)

Author keywords

Arc volcano; Degrees of melting; Mantle wedge; Water; Wet and dry basalts

Indexed keywords

BASALT; FRACTIONAL CRYSTALLIZATION; MAGMA CHEMISTRY; PARTIAL MELTING; PHENGITE; SEAFLOOR; VOLCANIC ERUPTION;

IZU-BONIN ARC; PACIFIC OCEAN;

EID: 34848925252     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egm048     Document Type: Article

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