Miocene dislocations during the formation of the Sea of Japan basin: Case study of Tsushima Island

V. V. Golozubov, S. A. Kasatkin, K. Yokoyama, Yu Tsutsumi, Shoichi Kiyokawa

研究成果: ジャーナルへの寄稿記事

1 引用 (Scopus)

抄録

Lower Miocene rocks of the Taishu Group accumulated in the Tsushima pull-apart graben, which downwarped and was filled with sediments at a particularly high rate (about 2700 m/Ma), in the background of northeastern regional shortening. A considerable part of the sedimentary prism is composed of material supplied by landslide blocks from the shallow shelf. Folding and penetration of granite intrusions on Tsushima Island occurred ca. 15 Ma ago, simultaneously with the main phase of opening of the Sea of Japan, in the field of different, northwestern shortening, which had a local character and was related to clockwise rotation of the Southwestern Japan block. These rotations in turn could have been the result of an intensive rifting episode in the Central and Honshu basins of the Sea of Japan, which are located north of Tsushima Island.

元の言語英語
ページ(範囲)412-427
ページ数16
ジャーナルGeotectonics
51
発行部数4
DOI
出版物ステータス出版済み - 7 1 2017

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dislocation
Miocene
basin
graben
rifting
folding
landslide
penetration
granite
rock
sediment
sea
rate
material

All Science Journal Classification (ASJC) codes

  • Geology

これを引用

Miocene dislocations during the formation of the Sea of Japan basin : Case study of Tsushima Island. / Golozubov, V. V.; Kasatkin, S. A.; Yokoyama, K.; Tsutsumi, Yu; Kiyokawa, Shoichi.

:: Geotectonics, 巻 51, 番号 4, 01.07.2017, p. 412-427.

研究成果: ジャーナルへの寄稿記事

Golozubov, V. V. ; Kasatkin, S. A. ; Yokoyama, K. ; Tsutsumi, Yu ; Kiyokawa, Shoichi. / Miocene dislocations during the formation of the Sea of Japan basin : Case study of Tsushima Island. :: Geotectonics. 2017 ; 巻 51, 番号 4. pp. 412-427.
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