Seismic velocity structure along the Sea of Japan with large events derived from seismic tomography for whole Japanese Islands including reflection survey data and NIED MOWLAS Hi-net and S-net data

Abstract We conducted seismic tomography for entire Japanese Islands including the Sea of Japan and the Pacific Ocean using arrival times from reflection survey as well as the routine seismic network. We successfully imaged the shallow zone along the Sea of Japan from offshore Yamagata to the Noto P...

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Main Authors: Makoto Matsubara, Tatsuya Ishiyama, Tetsuo No, Kenji Uehira, Masashi Mochizuki, Toshihiko Kanazawa, Narumi Takahashi, Shin’ichiro Kamiya
Format: Article
Language:English
Published: SpringerOpen 2022-11-01
Series:Earth, Planets and Space
Subjects:
Online Access:https://doi.org/10.1186/s40623-022-01724-0
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author Makoto Matsubara
Tatsuya Ishiyama
Tetsuo No
Kenji Uehira
Masashi Mochizuki
Toshihiko Kanazawa
Narumi Takahashi
Shin’ichiro Kamiya
author_facet Makoto Matsubara
Tatsuya Ishiyama
Tetsuo No
Kenji Uehira
Masashi Mochizuki
Toshihiko Kanazawa
Narumi Takahashi
Shin’ichiro Kamiya
author_sort Makoto Matsubara
collection DOAJ
description Abstract We conducted seismic tomography for entire Japanese Islands including the Sea of Japan and the Pacific Ocean using arrival times from reflection survey as well as the routine seismic network. We successfully imaged the shallow zone along the Sea of Japan from offshore Yamagata to the Noto Peninsula by using air gun data. An extremely low-V shallow zone is imaged between Sado Island and Noto Peninsula. We also obtained detailed seismic velocity structure beneath the Pacific Ocean at depths of 20–50 km using S-net data. The 2007 Noto Peninsula, the 2007 offshore Chuetsu, and the 2019 offshore Yamagata earthquakes occurred at the boundary between high-Vp and low-Vp zones. The west side of the hypocenter of the 2019 offshore Yamagata earthquake at depths of 10–30 km has high-V corresponding to the Mogami Trough. This high-V zone passes through Awa Island and reaches Sado Basin between Sado Island and Honshu. A major rift zone in the Tohoku Arc extending from the Akita region to the Niigata region along the coast of Sea of Japan corresponds to high-V lower crust and a shallow Moho. Graphical Abstract
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spelling doaj.art-7490363aa2114b04b43d07490d991dd02022-12-22T04:20:24ZengSpringerOpenEarth, Planets and Space1880-59812022-11-0174112710.1186/s40623-022-01724-0Seismic velocity structure along the Sea of Japan with large events derived from seismic tomography for whole Japanese Islands including reflection survey data and NIED MOWLAS Hi-net and S-net dataMakoto Matsubara0Tatsuya Ishiyama1Tetsuo No2Kenji Uehira3Masashi Mochizuki4Toshihiko Kanazawa5Narumi Takahashi6Shin’ichiro Kamiya7National Research Institute for Earth Science and Disaster ResilienceEarthquake Research Institute, The University of TokyoJapan Agency for Marine-Earth Science and TecnologyNational Research Institute for Earth Science and Disaster ResilienceNational Research Institute for Earth Science and Disaster ResilienceAssociation for the Development of Earthquake PredictionNational Research Institute for Earth Science and Disaster ResilienceNational Research Institute for Earth Science and Disaster ResilienceAbstract We conducted seismic tomography for entire Japanese Islands including the Sea of Japan and the Pacific Ocean using arrival times from reflection survey as well as the routine seismic network. We successfully imaged the shallow zone along the Sea of Japan from offshore Yamagata to the Noto Peninsula by using air gun data. An extremely low-V shallow zone is imaged between Sado Island and Noto Peninsula. We also obtained detailed seismic velocity structure beneath the Pacific Ocean at depths of 20–50 km using S-net data. The 2007 Noto Peninsula, the 2007 offshore Chuetsu, and the 2019 offshore Yamagata earthquakes occurred at the boundary between high-Vp and low-Vp zones. The west side of the hypocenter of the 2019 offshore Yamagata earthquake at depths of 10–30 km has high-V corresponding to the Mogami Trough. This high-V zone passes through Awa Island and reaches Sado Basin between Sado Island and Honshu. A major rift zone in the Tohoku Arc extending from the Akita region to the Niigata region along the coast of Sea of Japan corresponds to high-V lower crust and a shallow Moho. Graphical Abstracthttps://doi.org/10.1186/s40623-022-01724-0Seismic tomographySea of JapanFailed riftNIED S-netNIED Hi-net
spellingShingle Makoto Matsubara
Tatsuya Ishiyama
Tetsuo No
Kenji Uehira
Masashi Mochizuki
Toshihiko Kanazawa
Narumi Takahashi
Shin’ichiro Kamiya
Seismic velocity structure along the Sea of Japan with large events derived from seismic tomography for whole Japanese Islands including reflection survey data and NIED MOWLAS Hi-net and S-net data
Earth, Planets and Space
Seismic tomography
Sea of Japan
Failed rift
NIED S-net
NIED Hi-net
title Seismic velocity structure along the Sea of Japan with large events derived from seismic tomography for whole Japanese Islands including reflection survey data and NIED MOWLAS Hi-net and S-net data
title_full Seismic velocity structure along the Sea of Japan with large events derived from seismic tomography for whole Japanese Islands including reflection survey data and NIED MOWLAS Hi-net and S-net data
title_fullStr Seismic velocity structure along the Sea of Japan with large events derived from seismic tomography for whole Japanese Islands including reflection survey data and NIED MOWLAS Hi-net and S-net data
title_full_unstemmed Seismic velocity structure along the Sea of Japan with large events derived from seismic tomography for whole Japanese Islands including reflection survey data and NIED MOWLAS Hi-net and S-net data
title_short Seismic velocity structure along the Sea of Japan with large events derived from seismic tomography for whole Japanese Islands including reflection survey data and NIED MOWLAS Hi-net and S-net data
title_sort seismic velocity structure along the sea of japan with large events derived from seismic tomography for whole japanese islands including reflection survey data and nied mowlas hi net and s net data
topic Seismic tomography
Sea of Japan
Failed rift
NIED S-net
NIED Hi-net
url https://doi.org/10.1186/s40623-022-01724-0
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