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  1. 防災科研関係論文

Deep seismic reflection profiling across the Ou Backbone range, northern Honshu Island, Japan

https://nied-repo.bosai.go.jp/records/4413
https://nied-repo.bosai.go.jp/records/4413
d479a41b-8745-430b-a377-09e0fb3c2c14
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Deep seismic reflection profiling across the Ou Backbone range, northern Honshu Island, Japan
言語
言語 eng
著者 H Sato

× H Sato

en H Sato

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N Hirata

× N Hirata

en N Hirata

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T Iwasaki

× T Iwasaki

en T Iwasaki

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M Matsubara

× M Matsubara

en M Matsubara

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T Ikawa

× T Ikawa

en T Ikawa

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抄録
内容記述タイプ Other
内容記述 Knowledge of the crustal structure, especially the geometry of seismogenic faults, is key to understanding active tectonic processes and assessing the size and frequency of future earthquakes. To reveal the relationship between crustal structure and earthquake activity in northern Honshu Island, common midpoint (CMP) deep reflection profiling and earthquake observations by densely deployed seismic stations were carried Out across S the active reverse faults that bound the Ou Backbone range. The 40-km-long CMP profile. portray a relatively simple fault geometry within the seismogenic layer. The reverse faults merge at a midcrustal detachment just below the base of the seismogenic layer, producing a pop-up structure that forms the On Backbone range. The top of the reflective middle to lower crust (4.5 s in travel time (TWT)) nearly coincides with the bottom of seismogenic layer. The P-wave velocity structure and surface geology suggest that the bounding faults are Miocene normal faults that have been reactivated as reverse faults. (C) 2002 Elsevier Science B.V. All rights reserved.
言語 en
書誌情報 en : TECTONOPHYSICS

巻 355, 号 1-4, p. 41-52
出版者
言語 en
出版者 ELSEVIER SCIENCE BV
ISSN
収録物識別子タイプ ISSN
収録物識別子 0040-1951
DOI
関連識別子 10.1016/S0040-1951(02)00133-6
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