Two primary basalt magma types from northwest Rota-1 volcano, Mariana arc and its mantle diapir or mantle wedge plume

Journal of Petrology

Volumn 52, Issue 6, 2011, Pages 1143-1183

  Tamura, Y ^a   Ishizuka, O ^b   Stern, R J ^c   Shukuno, H ^a   Kawabata, H ^a   Embley, R W ^d   Hirahara, Y ^a   Chang, Q ^a   Kimura, J I ^a   Tatsumi, Y ^a   Nunokawa, A ^a   Bloomer, S H ^e  

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

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

^c UNIVERSITY OF TEXAS AT DALLAS   (United States)

^d NOAA PACIFIC MARINE ENVIRONMENTAL LABORATORY   (United States)

^e OREGON STATE UNIVERSITY   (United States)

Author keywords

Arc volcano; Dry melting; Hydrous melting; Magma genesis; Mantle wedge; Primary magma; Subduction zone

Indexed keywords

BASALT; DIAPIR; LEAD ISOTOPE; MAGMA; MANTLE STRUCTURE; MELTING; NEODYMIUM ISOTOPE; PERIDOTITE; PETROGRAPHY; PHENOCRYST; STRONTIUM ISOTOPE; SUBDUCTION ZONE;

EID: 79959578398     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egr022     Document Type: Article

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