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  1. 防災科研関係論文

A Shallow Crustal Structure as Derived from an Explosion Seismic Experiment

https://nied-repo.bosai.go.jp/records/5829
https://nied-repo.bosai.go.jp/records/5829
10718ab8-612a-4d47-a4b9-2d1ed81ccc42
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル A Shallow Crustal Structure as Derived from an Explosion Seismic Experiment
言語
言語 eng
著者 Akira Ikami

× Akira Ikami

en Akira Ikami

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Akira Ikami

× Akira Ikami

en Akira Ikami

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Kazuki Koketsu

× Kazuki Koketsu

en Kazuki Koketsu

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Shuzo Asano

× Shuzo Asano

en Shuzo Asano

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Shuzo Asano

× Shuzo Asano

en Shuzo Asano

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Takeo Moriya

× Takeo Moriya

en Takeo Moriya

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Kiyoshi Ito

× Kiyoshi Ito

en Kiyoshi Ito

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Kiyoshi Ito

× Kiyoshi Ito

en Kiyoshi Ito

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Toshikazu Tanada

× Toshikazu Tanada

en Toshikazu Tanada

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Kazumasa Yoshida

× Kazumasa Yoshida

en Kazumasa Yoshida

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Kazumasa Yoshida

× Kazumasa Yoshida

en Kazumasa Yoshida

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Toshikazu Tanada

× Toshikazu Tanada

en Toshikazu Tanada

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Tetsuichiro Yabuki

× Tetsuichiro Yabuki

en Tetsuichiro Yabuki

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Naoshi Hirata

× Naoshi Hirata

en Naoshi Hirata

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Naoshi Hirata

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en Naoshi Hirata

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抄録
内容記述タイプ Other
内容記述 The key subjects of the 1986 Joint Seisrnological Research in Western Nagano Prefecture (JSR'86) were to determine hypocenters of aftershocks of the 1984 Western Nagano Prefecture Earthquake and the shallow crustal structure precisely. Therefore, we deployed a temporary seismic network of closely spaced stations with a high quality in the southern foot of Mt. Ontake, the epicentral area of the 1984 earthquake. As one of the key subjects of JSR'86, a three-dimensional velocity modeling was executed using the natural earthquake data observed during the experiment. In addition to this inversion of observed data of earthquakes, we conducted an explosion seismic experiment to obtain information on the shallow crustal structure more precisely to improve hypocenter determination as well as to find characteristics of the structure. The two-dimensional profile was derived from observed data of seismic waves by two shots at 43 temporal stations. The length of the profile was 20 km, crossing the Otaki River which may be concordant with the structural boundary as pointed out geologically and topographically. The derived time-term distribution represents the two-dimensiqnal surface-layer thickness, and has correlations to the distribution of the Bouguer gravity anomaly and the hypocenter distribution in the area. The rim of high consistency of contour lines on the Bouguer gravity anomaly map and the time-term distribution map may coincide with the boundary of the seismically active area. c 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. 361-377, 発行日 1992
出版者
言語 en
出版者 CENTER ACADEMIC PUBL JAPAN
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/jpe1952.40.361
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