Origin of the early Cenozoic belt boundary thrust and Izanagi–Pacific ridge subduction in the western Pacific margin

The belt boundary thrust within the Cretaceous–Neogene accretionary complex of the Shimanto Belt, southwestern Japan, extends for more than ~ 1 000 km along the Japanese islands. A common understanding of the origin of the thrust is that it is an out of sequence thrust as a result of continuous accr...

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Bibliographic Details
Main Authors: Kimura, Gaku, Kitamura, Yujin, Yamaguchi, Asuka, Kameda, Jun, Hashimoto, Yoshitaka, Hamahashi, Mari
Other Authors: Earth Observatory of Singapore
Format: Article
Language:English
Published: 2019
Subjects:
Online Access:https://hdl.handle.net/10356/90311
http://hdl.handle.net/10220/50479
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Institution: Nanyang Technological University
Language: English