Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Kenji Kanjo"'
Publikováno v:
Journal of Volcanology and Geothermal Research. 311:72-78
Although analytical expressions for deformation due to simple reservoirs and planar dikes have been in use for decades, seldom are there sufficient data to provide well-constrained detailed models of volcanic activity. Deformation due to the eruption
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14b7fce5ff28a94bcf333e9891705929
https://doi.org/10.1016/j.jvolgeores.2016.01.001
https://doi.org/10.1016/j.jvolgeores.2016.01.001
Publikováno v:
Zisin (Journal of the Seismological Society of Japan. 2nd ser.). 66:27-30
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61576c1635fb88e83ea2ac0207015a65
https://doi.org/10.4294/zisin.66.27
https://doi.org/10.4294/zisin.66.27
Publikováno v:
Physics of the Earth and Planetary Interiors. 146:101-112
Previous seismic studies for southeastern Asia around Indonesia have used global seismic data and thus included few regional broadband seismic stations. To better understand seismic structure of this area, we temporarily deployed Japan–Indonesia Se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b563e349816048aa6dde374eb897c768
https://doi.org/10.1016/j.pepi.2003.06.009
https://doi.org/10.1016/j.pepi.2003.06.009
Autor:
Satoshi Kaneshima, Kenji Kanjo, Yasushi Ishihara, Shoji Sekiguchi, Toshiki Ohtaki, Takeshi Nishimura, Purwana Ibnu
Publikováno v:
BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN. 53:445-459
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81c8901e5d1af1dd47f3fa119312bace
https://doi.org/10.9795/bullgsj.53.445
https://doi.org/10.9795/bullgsj.53.445
Publikováno v:
Journal of Geophysical Research: Solid Earth. 106:13485-13499
An outstanding slow wave train similar to T wave in appearance has been observed on records of an ocean bottom seismometer array, off Boso, central Japan. These slow wave trains are not observed on land, are usually spindle-shaped and dominant in ver
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ead2d2f9c08f635cd4d04c7482e9b8f2
https://doi.org/10.1029/2000jb900476
https://doi.org/10.1029/2000jb900476
Autor:
Yushiro Fujii, Toshiki Ohtaki, Tomoharu Saita, Hiroshi Takenaka, Satoshi Harada, Kenji Kanjo, Yasushi Ishihara, Satoshi Kaneshima, Yasuhiro Yoshida, Kenji Fujiwara, Akiko Tanaka, Shinichiro Kamiya, Daisuke Suetsugu
Publikováno v:
Zisin (Journal of the Seismological Society of Japan. 2nd ser.). 54:9-16
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::60e3bac314c378ccb9fc3b0972ab0d55
https://doi.org/10.4294/zisin1948.54.1_9
https://doi.org/10.4294/zisin1948.54.1_9
Publikováno v:
Geophysical Journal International. 142:361-370
Summary On 1996 September 4, a submarine earthquake occurred underneath the Smith Caldera near Tori-Shima on the Izu-Bonin arc, Japan. Its mechanism was a CLVD with the principal tensile dipole in the vertical direction. The tsunami magnitude Mt of 7
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::892db7f9caf9243c998bf80e18369551
https://doi.org/10.1046/j.1365-246x.2000.00153.x
https://doi.org/10.1046/j.1365-246x.2000.00153.x
Publikováno v:
Journal of Geophysical Research: Solid Earth. 105:443-462
The sequential process of the 1986 Izu-Oshima volcano eruption, Japan, was recorded by a volumetric strain meter near the erupted summit. The records show occasional strain offsets accompanying long-period damped oscillations, which we interpret as r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7854e008883eb3a7d56a4ce1d5c8f2cc
https://doi.org/10.1029/1999jb900367
https://doi.org/10.1029/1999jb900367
Publikováno v:
Geophysical Research Letters. 25:105-108
Freely damped oscillations associated with strain offsets were observed by a nearby volumetric strainmeter during the 1986 Izu-Oshima Volcano eruption, Japan. These events are interpreted as a response of the magma-filled conduit to step-like changes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b21c891c78b0afa3b01f860eefb26308
https://doi.org/10.1029/97gl03352
https://doi.org/10.1029/97gl03352
Publikováno v:
Geophysical Research Letters. 24:691-694
The water level in an observation well (EDY) has been monitored with high frequency sampling (1/sec). Large changes in the water level are observed in this well, which correspond to dynamic strain changes due to the passage of long period seismic wav
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::efd2121d46b36c2db73dfdd74e670ad1
https://doi.org/10.1029/97gl00471
https://doi.org/10.1029/97gl00471