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  1. 防災科研関係論文

Structures and active tectonics of compressionally reactivated back-arc failed rift across the Toyama trough in the Sea of Japan, revealed by multiscale seismic profiling

https://nied-repo.bosai.go.jp/records/2823
https://nied-repo.bosai.go.jp/records/2823
0f5db7de-13d4-4e24-ad43-8b11173f18c3
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Structures and active tectonics of compressionally reactivated back-arc failed rift across the Toyama trough in the Sea of Japan, revealed by multiscale seismic profiling
言語
言語 eng
著者 Tatsuya Ishiyama

× Tatsuya Ishiyama

en Tatsuya Ishiyama

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Hiroshi Sato

× Hiroshi Sato

en Hiroshi Sato

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Naoko Kato

× Naoko Kato

en Naoko Kato

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Shin Koshiya

× Shin Koshiya

en Shin Koshiya

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Susumu Abe

× Susumu Abe

en Susumu Abe

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Kazuya Shiraishi

× Kazuya Shiraishi

en Kazuya Shiraishi

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Makoto Matsubara

× Makoto Matsubara

en Makoto Matsubara

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抄録
内容記述タイプ Other
内容記述 Compressional reactivation of back-arc failed rifts in the Sea of Japan and its mechanism that mobilizes active tectonics based on the crustal structures remains poorly understood. Here, we show new results and interpretations of onshore-offshore deep seismic reflection profiles across the Toyama trough and its southern extension, located in the Sea of Japan back-arc rift, to reveal their deep to shallow structures of the crust and reactivated active faults. We observed (1) approximately 5 km thick, syn- and post-rift Neogene sediments underlain by pre-Neogene basement rocks characterized by high velocity anomalies, and (2) crustal thrust wedges adjacent to the rift axis. Shallower high-resolution seismic reflection profiles also suggest Quaternary structural growth of the reactivated thrusts and thrust wedges, consistent with tectonic geomorphology of the middle to late Pleistocene marine and fluvial terraces. These findings demonstrate that the mechanical contrasts between the crustal thrust wedges, primarily composed of the pre-rift continental crust and high velocity lower crust caused by mafic intrusions in the rifting stage, have fundamentally controlled the styles of active deformation during the post-rift Quatemary compressional stress regime. These results also contribute to the construction of the seismic source fault models for tsunamis and seismic hazard estimations of this region. In addition, we emphasize that combining multi-scale seismic reflection profiles with tectonic geomorphology sheds light on complicated structural characteristics and recent activities of reactivated normal faults that are mostly blind because of the dynamic subsidence of failed rift structures. (C) 2016 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : TECTONOPHYSICS

巻 710, p. 21-36, 発行日 2017-07
出版者
言語 en
出版者 ELSEVIER SCIENCE BV
ISSN
収録物識別子タイプ EISSN
収録物識別子 1879-3266
DOI
関連識別子 10.1016/j.tecto.2016.09.029
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