P-wave velocity structure of Usu volcano: Implication of structural controls on magma movements and eruption locations

Journal of Volcanology and Geothermal Research

Volumn 160, Issue 1-2, 2007, Pages 175-194

  Onizawa, Shin'ya ^a   Oshima, Hiromitsu ^a   Aoyama, Hiroshi ^a   Mori, Hitoshi Y ^a   Maekawa, Tokumitsu ^a   Suzuki, Atsuo ^a   Tsutsui, Tomoki ^b   Matsuwo, Norimichi ^c   Oikawa, Jun ^d   Ohminato, Takao ^d   Yamamoto, Keigo ^e   Mori, Takehiko ^f   Taira, Taka'aki ^a   Miyamachi, Hiroki ^g   Okada, Hiromu ^a  

^a HOKKAIDO UNIVERSITY   (Japan)

^b AKITA UNIVERSITY   (Japan)

^c KYUSHU UNIVERSITY   (Japan)

^d UNIVERSITY OF TOKYO   (Japan)

^e KYOTO UNIVERSITY   (Japan)

^f TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

^g KAGOSHIMA UNIVERSITY   (Japan)

Author keywords

eruption location; magma movement; precursory earthquake; subsurface structure; Usu volcano; velocity structure

Indexed keywords

EARTHQUAKE EFFECTS; SEISMIC WAVES; SEISMOLOGY; VELOCITY;

MAGMA MOVEMENT; P-WAVE VELOCITY STRUCTURE; PRECURSORY EARTHQUAKE; SUBSURFACE STRUCTURE; USU VOLCANO;

VOLCANOES;

BASEMENT ROCK; CRATER; EARTHQUAKE; GEOGRAPHICAL DISTRIBUTION; P-WAVE; SEISMIC DATA; STRUCTURAL CONTROL; VELOCITY STRUCTURE; VOLCANIC ERUPTION; VOLCANO;

ASIA; EURASIA; FAR EAST; HOKKAIDO; JAPAN; MOUNT USU;

EID: 33845941975     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2006.10.005     Document Type: Article

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