Active-source seismic experiment confirms the magma pathway of Mount Asama, Japan

Eos

Volumn 90, Issue 50, 2009, Pages 482-483

  Aokl, Yosuke ^a   Takeo, Mlnoru ^a   Mortta, Yuichi ^a   Tsutsui, Tomokl ^b  

^a UNIVERSITY OF TOKYO   (Japan)

^b AKITA UNIVERSITY   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

EXPERIMENTAL STUDY; EXPLOSIVE VOLCANISM; LAVA FLOW; MAGMATISM; SEISMICITY; VOLCANISM;

ASAMA VOLCANO; CHUBU; HONSHU; JAPAN; NAGANO;

EID: 77749302111     PISSN: 00963941     EISSN: None     Source Type: Journal    
DOI: 10.1029/2009EO500002     Document Type: Short Survey

References (5)

1. Aoki, Y., et al. (2009), P-wave velocity structure beneath Asama volcano, Japan, inferred from active source seismic experiment, J. Volcanol. Geotherm. Res., 187, 272-277.
2. Onizawa, S., et al. (2007), P-wave velocity structure of Usu volcano: Implication of structural controls on magma movements and eruption locations, J. Volcanol. Geotherm. Res., 160, 175-194.
3. Takeo, M., Y. Aoki, T. Ohminato, and M. Yamamoto (2006), Magma supply path beneath Mount Asama volcano, Japan, Geophys. Res. Lett., 33, L15310, doi:10.1029/2006GL026247.
4. Zollo, A., et al. (1996), Seismic evidence for a lowvelocity zone in the upper crust beneath Mount Vesuvius, Science, 274, 592-594.
5. Zollo, A., et al. (1998), An image of Mt. Vesuvius obtained by 2D seismic tomography, J. Volcanol. Geotherm. Res., 82, 161-174.