TY - JOUR
T1 - Seismic reflection survey of the crustal structure beneath Unzen volcano, Kyushu, Japan
AU - Matsumoto, Satoshi
AU - Shimizu, Hiroshi
AU - Onishi, Masazumi
AU - Uehira, Kenji
N1 - Funding Information:
Acknowledgments. We wish to thank all the staff and students of the Institute of Seismology and Volcanology, Kyushu University, who helped in carrying out this survey. We are grateful to the anonymous reviewers for their insightful and critical discussion of this paper. We also thank Drs. Uraki and Higashinaka of the Japex Geoscience Institute for their efforts in carrying out the reflection analysis. We are grateful to Dr. Umakoshi for his valuable comments and discussions and for giving us access to hypocenter data. This study was supported by Unzen Scientific Drilling Project, funded by the Ministry of Education, Culture, Sports, Science and Technology, Japan.
PY - 2012
Y1 - 2012
N2 - Unzen volcano is located in the western part of Kyushu, Japan. We carried out a seismic reflection survey at Unzen volcano in order to elucidate the structure of the volcano. Although the survey was conducted in a volcanic area under difficult conditions, such as artificial noises and a complex structure, we were able to resolve the structure beneath the profile using vibrator sources and a large number of stacking signals. The processed depth sections confirmed that Unzen volcano developed in a graben structure, as has been suggested in other geological studies. We imaged many subsurface normal faults shallower than 1 km. These faults, mostly covered with volcanic lava and deposits, were identified at the surface. Strong reflectors were found at a depth of approximately 3 km. They were located just above the pressure source of the latest eruption, as inferred from geodetic data. The geometric relationship between the reflection image, the pressure source location, and the lava dome suggests that the conduit from the lava dome could connect to the magma chamber located 4 km away from the lava dome.
AB - Unzen volcano is located in the western part of Kyushu, Japan. We carried out a seismic reflection survey at Unzen volcano in order to elucidate the structure of the volcano. Although the survey was conducted in a volcanic area under difficult conditions, such as artificial noises and a complex structure, we were able to resolve the structure beneath the profile using vibrator sources and a large number of stacking signals. The processed depth sections confirmed that Unzen volcano developed in a graben structure, as has been suggested in other geological studies. We imaged many subsurface normal faults shallower than 1 km. These faults, mostly covered with volcanic lava and deposits, were identified at the surface. Strong reflectors were found at a depth of approximately 3 km. They were located just above the pressure source of the latest eruption, as inferred from geodetic data. The geometric relationship between the reflection image, the pressure source location, and the lava dome suggests that the conduit from the lava dome could connect to the magma chamber located 4 km away from the lava dome.
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U2 - 10.5047/eps.2011.11.006
DO - 10.5047/eps.2011.11.006
M3 - Article
AN - SCOPUS:84876399886
SN - 1343-8832
VL - 64
SP - 405
EP - 414
JO - Earth, Planets and Space
JF - Earth, Planets and Space
IS - 5
ER -