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Since Paleogene, this region has experienced the dextral oblique transpression between the Eurasia and North American (Okhotsk) Plates and the subsequent collision between the Northeast Japan Arc and the Kuril Arc due to the oblique subduction of the Pacific Plate. This earthquake occurred beneath the foreland fold-and-thrust belt of the Hidaka Collision zone developed by the collision process, and is characterized by its deep focal depth (~ 37?km) and complicated rupture process. The reanalyses of controlled source seismic data collected in the 1998?2000 Hokkaido Transect Project revealed the detailed structure beneath the fold-and-thrust belt, and its relationship with the aftershock activity of this earthquake. Our reflection processing using the CRS/MDRS stacking method imaged for the first time the lower crust and uppermost mantle structures of the Northeast Japan Arc underthrust beneath a thick (~ 5?10?km) sedimentary package of the fold-and-thrust belt. 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  1. 防災科研関係論文

Structural heterogeneity in and around the fold-and-thrust belt of the Hidaka Collision zone, Hokkaido, Japan and its relationship to the aftershock activity of the 2018 Hokkaido Eastern Iburi Earthquake

https://nied-repo.bosai.go.jp/records/3109
https://nied-repo.bosai.go.jp/records/3109
ce629e4c-8558-4d5f-813e-5bc366dbb040
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Structural heterogeneity in and around the fold-and-thrust belt of the Hidaka Collision zone, Hokkaido, Japan and its relationship to the aftershock activity of the 2018 Hokkaido Eastern Iburi Earthquake
タイトル
言語 en
タイトル Structural heterogeneity in and around the fold-and-thrust belt of the Hidaka Collision zone, Hokkaido, Japan and its relationship to the aftershock activity of the 2018 Hokkaido Eastern Iburi Earthquake
言語
言語 eng
著者 Iwasaki, T

× Iwasaki, T

ja Iwasaki, T

en Iwasaki, T

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N. Tsumura

× N. Tsumura

ja N. Tsumura

en N. Tsumura

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T. Ito

× T. Ito

ja T. Ito

en T. Ito

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K. Arita

× K. Arita

ja K. Arita

en K. Arita

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M. Matsubara

× M. Matsubara

ja M. Matsubara

en M. Matsubara

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H. Sato

× H. Sato

ja H. Sato

en H. Sato

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E. Kurashimo

× E. Kurashimo

ja E. Kurashimo

en E. Kurashimo

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N. Hirata

× N. Hirata

ja N. Hirata

en N. Hirata

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S. Abe

× S. Abe

ja S. Abe

en S. Abe

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K. Noda

× K. Noda

ja K. Noda

en K. Noda

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A. Fujiwara

× A. Fujiwara

ja A. Fujiwara

en A. Fujiwara

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S. Kikuchi

× S. Kikuchi

ja S. Kikuchi

en S. Kikuchi

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K. Suzuki

× K. Suzuki

ja K. Suzuki

en K. Suzuki

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抄録
内容記述タイプ Other
内容記述 The Hokkaido Eastern Iburi Earthquake (M = 6.7) occurred on Sep. 6, 2018 in the southern part of Central Hokkaido, Japan. Since Paleogene, this region has experienced the dextral oblique transpression between the Eurasia and North American (Okhotsk) Plates and the subsequent collision between the Northeast Japan Arc and the Kuril Arc due to the oblique subduction of the Pacific Plate. This earthquake occurred beneath the foreland fold-and-thrust belt of the Hidaka Collision zone developed by the collision process, and is characterized by its deep focal depth (~ 37?km) and complicated rupture process. The reanalyses of controlled source seismic data collected in the 1998?2000 Hokkaido Transect Project revealed the detailed structure beneath the fold-and-thrust belt, and its relationship with the aftershock activity of this earthquake. Our reflection processing using the CRS/MDRS stacking method imaged for the first time the lower crust and uppermost mantle structures of the Northeast Japan Arc underthrust beneath a thick (~ 5?10?km) sedimentary package of the fold-and-thrust belt. Based on the analysis of the refraction/wide-angle reflection data, the total thickness of this Northeast Japan Arc crust is only 16?22?km. The Moho is at depths of 26?28?km in the source region of the Hokkaido Eastern Iburi Earthquake. Our hypocenter determination using a 3D structure model shows that most of the aftershocks are distributed in a depth range of 7?45?km with steep geometry facing to the east. The seismic activity is quite low within the thick sediments of the fold?thrust belt, from which we find no indication on the relationship of this event with the shallow (< 10?15?km) and rather flat active faults developed in the fold-and-thrust belt. On the other hand, a number of aftershocks are distributed below the Moho. This high activity may be caused by the cold crust delaminated from the Kuril Arc side by the arc?arc collision, which prevents the thermal circulation and cools the forearc uppermost mantle to generate an environment more favorable for brittle fracture. [Figure not available: see fulltext.].
言語 en
書誌情報 ja : Earth, Planets and Space
en : Earth, Planets and Space

巻 71, 号 1, p. 1-19, 発行日 2019-06
ISSN
収録物識別子タイプ EISSN
収録物識別子 1880-5981
DOI
関連識別子 10.1186/s40623-019-1081-z
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