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  1. 防災科研関係論文

Three-Dimensional P and S Wave Velocity Structure in the Focal Region of the 1984 Western Nagano Prefecture Earthquake

https://nied-repo.bosai.go.jp/records/6602
https://nied-repo.bosai.go.jp/records/6602
b184f48f-0e26-4312-9de1-e04e9c310efd
Item type researchmap(1)
公開日 2024-05-06
タイトル
言語 en
タイトル Three-Dimensional P and S Wave Velocity Structure in the Focal Region of the 1984 Western Nagano Prefecture Earthquake
言語
言語 eng
著者 Hiroo Wada

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Fumiaki Takeuchi

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en Fumiaki Takeuchi

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Takeshi Mikumo

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Yuji Kurata

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Satoru Kuriyama

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Makoto Koizumi

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Kazuro Hirahara

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Norio Hirano

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Satoshi Kaneshima

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Toru Nakamura

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Kinya Nishigami

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Kazuo Oike

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Takuo Shibutani

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Takahiro Okura

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Naoshi Hirata

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Toshihiko Kanazawa

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Shoji Tomita

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Tetsuichiro Yabuki

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Tooru Ooida

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Akira Ikami

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Masaru Nakamura

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Harumi Aoki

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Iwao Fujii

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Rikio Miyajima

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Mamoru Yamada

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Fumihito Yamazaki

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Akira Ikami

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Sadaomi Suzuki

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Akihiko Yamamoto

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Takeo Moriya

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Hiroki Miyamachi

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Ken-Ichiro Yamashina

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Kaname Sakai

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Megumi Mizoue

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Toshio Haneda

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Masayoshi Takahashi

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Tameshige Tsukuda

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Shin-Ichi Hashimoto

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Yukio Ishiketa

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Ikuo Karakama

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Masaru Kobayashi

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Katsumi Miura

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Isao Nakamura

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Akio Takagi

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Toshio Kono

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Akira Hasegawa

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Shigeki Horiuchi

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Toru Matsuzawa

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Yasuhiro Umeda

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Yoshihisa Iio

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Kiyoshi Ito

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Akio Kuroiso

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Tatsuo Saeki

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Akihiko Ito

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Masahiro Kosuga

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Kazuaki Miura

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Atsushi Nakajima

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Masayuki Suzuki

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Toshio Mitsunami

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Takuo Okamoto

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Toru Ouchi

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Toshikazu Tanada

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Manabu Yokohama

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抄録
内容記述タイプ Other
内容記述 The detailed three-dimensional P and S wave velocity structure in the focal region of the 1984 Western Nagano Prefecture Earthquake occurring close to an active volcano, Mt. Ontake, central Japan, is derived from a tomographic inversion of travel time data obtained by the 1986 Joint Seismological Research in Western Nagano Prefecture. The data set includes 7,693 P-wave and 6,070 S-wave arrival times observed at 49 stations from 212 local earthquakes and 2 explosions. The velocities in the shallow portion of upper crust are determined at each grid point with its spacing of 1-2 km and good resolutions are obtained from the Earth's surface to a depth of 4 km. There exist strong lateral heterogeneities especially from the surface to a depth of 1 km. The seismic velocity map obtained in the height of 1 km above sea level well corresponds to the maps of surface geology and Bouguer gravity anomaly. This correspondence, however, is not so clear in the deeper layers. And, the greater the depth, the less heterogeneous the velocity structure. The velocity distribution on the fault seems to correspond to the distribution of dislocation and rupture front estimated from an analysis of strong motion and geodetic data: the low velocity region has the large amount of dislocation and the retarded rupture front. © 1992, The Seismological Society of Japan, The Volcanological Society of Japan, The Geodetic Society of Japan. All rights reserved.
言語 en
書誌情報 en : Journal of Physics of the Earth

巻 40, 号 2, p. 343-360, 発行日 1992
ISSN
収録物識別子タイプ ISSN
収録物識別子 0022-3743
DOI
関連識別子 10.4294/jpe1952.40.343
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