Depth and evolution of a silicic magma chamber: Melting experiments on a low-K rhyolite from Usu volcano, Japan

Journal of Petrology

Volumn 51, Issue 6, 2010, Pages 1333-1354

  Tomiya, Akihiko ^a   Takahashi, Eiichi ^b   Furukawa, Noboru ^c   Suzuki, Toshihiro ^d  

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

^b TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

^c CHIBA UNIVERSITY   (Japan)

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

Author keywords

Magma chamber; Neutral buoyancy; Plagioclase; Plinian eruption; Pre eruptive P Tcondition

Indexed keywords

BUOYANCY; CHEMICAL COMPOSITION; CRYSTALLIZATION; EMPLACEMENT; HYDROUS MINERAL; MAGMA CHAMBER; MELTING; P-T CONDITIONS; PHASE EQUILIBRIUM; PLAGIOCLASE; PLINIAN ERUPTION; PUMICE; RHYOLITE;

HOKKAIDO; JAPAN; MOUNT USU;

PLINIA;

EID: 77954020011     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egq021     Document Type: Article

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