Evolution of the magma chamber beneath Usu volcano since 1663: A natural laboratory for observing changing phenocryst compositions and textures

Journal of Petrology

Volumn 46, Issue 12, 2005, Pages 2395-2426

  Tomiya, Akihiko ^a   Takahashi, Eiichi ^b  

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

^b TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

Author keywords

Continuous existence of magma chamber; Dacite; Dissolution and diffusion of phenocrysts; Magma mixing; Magnetite

Indexed keywords

DACITE; MAGMA CHAMBER; MAGNETITE; MIXING; PHENOCRYST;

ASIA; EASTERN HEMISPHERE; EURASIA; FAR EAST; HOKKAIDO; JAPAN; MOUNT USU; WORLD;

EID: 27944467148     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egi057     Document Type: Article

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