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...
| Auteurs principaux: | , , , , , |
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| Autres auteurs: | |
| Format: | Journal Article |
| Langue: | English |
| Publié: |
2019
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| Sujets: | |
| Accès en ligne: | https://hdl.handle.net/10356/90311 http://hdl.handle.net/10220/50479 |