Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Kentaro Kaneda"'
Autor:
Azusa Nishizawa, Kentaro Kaneda, Mitsuhiro Oikawa, Daishi Horiuchi, Yukari Fujioka, Chiaki Okada
Publikováno v:
Earth, Planets and Space, Vol 71, Iss 1, Pp 1-26 (2019)
Abstract The Okinawa Trough, to the southwest of Kyusyu, Japan, is an active backarc basin of the Ryukyu (Nansei-Shoto) island arc–trench system caused by the Philippine Sea plate subduction. Unlike other backarc basins around Japan, the Okinawa Tr
Externí odkaz:
https://doaj.org/article/7d4554223fbb4f5d900b4753d484a86c
Autor:
Azusa Nishizawa, Kentaro Kaneda, Mitsuhiro Oikawa, Daishi Horiuchi, Yukari Fujioka, Chiaki Okada
Publikováno v:
Earth, Planets and Space, Vol 69, Iss 1, Pp 1-17 (2017)
Abstract The Ryukyu (Nansei-Shoto) island arc-trench system, southwest of Japan, is formed by the subduction of the Philippine Sea (PHS) plate. Among the subduction zones surrounding the Japan Islands, the Ryukyu arc-trench system is unique in that i
Externí odkaz:
https://doaj.org/article/54b9561bce1740b89e584d0d24595c82
Autor:
Yoshihiko Tamura, Mathieu Rospabé, Gou Fujie, Akane Ohira, Kentaro Kaneda, Alexander R. L. Nichols, Georges Ceuleneer, Tomoki Sato, Shuichi Kodaira, Seiichi Miura, Eiichi Takazawa
Publikováno v:
Island Arc
Island Arc, 2022, 31 (1), ⟨10.1111/iar.12460⟩
Island Arc (1038-4871) (Wiley), 2022-01, Vol. 31, N. 1, P. e12460 (17p.)
Island Arc, 2022, 31 (1), ⟨10.1111/iar.12460⟩
Island Arc (1038-4871) (Wiley), 2022-01, Vol. 31, N. 1, P. e12460 (17p.)
It is common knowledge that the Moho is the boundary between the crust and the Earth's mantle. Here we show along several seismic profiles through the Pacific Plate that a correlation exists between the strength of Moho reflections, crustal thickness
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cc9f549294d8b52c204056383b5c7be9
https://hal.science/hal-03807990/document
https://hal.science/hal-03807990/document
Autor:
Daishi Horiuchi, Chiaki Okada, Mitsuhiro Oikawa, Yukari Fujioka, Kentaro Kaneda, Azusa Nishizawa
Publikováno v:
Earth, Planets and Space, Vol 71, Iss 1, Pp 1-26 (2019)
The Okinawa Trough, to the southwest of Kyusyu, Japan, is an active backarc basin of the Ryukyu (Nansei-Shoto) island arc–trench system caused by the Philippine Sea plate subduction. Unlike other backarc basins around Japan, the Okinawa Trough, ~ 1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cbba100f67c6d0dd8af5435d50587134
http://link.springer.com/article/10.1186/s40623-019-0998-6
http://link.springer.com/article/10.1186/s40623-019-0998-6
Publikováno v:
Journal of Geography (Chigaku Zasshi). 124:787-811
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2fedbe149a9eb626cc73d55150b78b70
https://doi.org/10.5026/jgeography.124.787
https://doi.org/10.5026/jgeography.124.787
Publikováno v:
Earth, Planets and Space. 61:e37-e40
P-wave velocity models related to the Philippine Sea plate subduction have been obtained from seismic explorations at the northern end of the Nansei-Shoto (Ryukyu) Trench. Both multi-channel seismic reflection and ocean bottom seismographic records p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3f506afd7d4e7a810c1c4a1330cc70b0
https://doi.org/10.1186/bf03352942
https://doi.org/10.1186/bf03352942
Publikováno v:
Earth, Planets and Space. 61:e5-e8
We present detailed P-wave velocity models of subducting seamounts from two wide-angle seismic experiments across the Erimo Seamount and Daiichi-Kashima Seamount, northern and southern ends of the Japan Trench. Common characteristics of the velocity
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f430294ef81feb934e38d652130b2161
https://doi.org/10.1186/bf03352912
https://doi.org/10.1186/bf03352912
Autor:
Kentaro Kaneda, Fuminori Honda, Junzo Kasahara, Eiichiro Nishiyama, Yoshihiro Naito, Nobutaka Oikawa, Aya Kamimura, Tamura Yasuo, Azusa Nishizawa, Ryuji Kubota, Kayoko Tsuruga
Publikováno v:
Exploration Geophysics. 39:1-14
We present a method for interpreting seismic records with arrivals and waveforms having characteristics which could be generated by extremely inhomogeneous velocity structures, such as non-typical oceanic crust, decollement at subduction zones, and s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::30f1bb6fc6b874e613a52fdd10e575e5
https://doi.org/10.1071/eg08004
https://doi.org/10.1071/eg08004
Autor:
Azusa Nishizawa, Ryuji Kubota, Kentaro Kaneda, Jun Ando, Junzo Kasahara, Atsushi Oshida, Eiichiro Nishiyama
Publikováno v:
Exploration Geophysics. 39:15-25
Ocean-bottom seismometer (OBS) positions are one of the key parameters in an OBS-airgun seismic survey for crustal structure study. To improve the quality of these parameters, we have developed a new method of determining OBS positions, using airgun
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8082484ed275fc483b7a589a125cbc2d
https://doi.org/10.1071/eg08005
https://doi.org/10.1071/eg08005
Publikováno v:
Earth, Planets and Space. 58:e33-e36
Wide-angle refraction experiments were conducted to reveal the crustal structure at the transition between the intra-oceanic island arc crust of the mid Izu-Ogasawara (Bonin) arc and the backarc oceanic crust of the Shikoku Basin. The island arc crus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d15313c4b0168f569dd92e1b4167cc4a
https://doi.org/10.1186/bf03352594
https://doi.org/10.1186/bf03352594