The subduction history of the Paleo-Pacific Oceanic plate from the Mesozoic to early Cenozoic in NE China and Sikhote-Alin, Russian Far East
The subduction of the Paleo-Pacific oceanic plate in NE China was probably initiated ca. 250 Ma ago. The Mudanjiang Ocean was closed between the Late Jurassic and Early Cretaceous. After that, the roll-back of the Paleo-Pacific oceanic plate and large-scale sinistral strike-slip faulting dominated...
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| Format: | Thesis |
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Curtin University
2021
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| Online Access: | http://hdl.handle.net/20.500.11937/84145 |
| _version_ | 1848764620411502592 |
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| author | Liu, Kai |
| author_facet | Liu, Kai |
| author_sort | Liu, Kai |
| building | Curtin Institutional Repository |
| collection | Online Access |
| description | The subduction of the Paleo-Pacific oceanic plate in NE China was probably initiated ca. 250 Ma ago. The Mudanjiang Ocean was closed between the Late Jurassic and Early Cretaceous. After that, the roll-back of the Paleo-Pacific oceanic plate and large-scale sinistral strike-slip faulting dominated the tectonics of the NE Asian continental margin. During the early Cenozoic, subduction of the Izanagi-Pacific ridge was subducted extended from SW Japan to Sikhote-Alin. |
| first_indexed | 2025-11-14T11:22:15Z |
| format | Thesis |
| id | curtin-20.500.11937-84145 |
| institution | Curtin University Malaysia |
| institution_category | Local University |
| last_indexed | 2025-11-14T11:22:15Z |
| publishDate | 2021 |
| publisher | Curtin University |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | curtin-20.500.11937-841452021-06-21T01:11:05Z The subduction history of the Paleo-Pacific Oceanic plate from the Mesozoic to early Cenozoic in NE China and Sikhote-Alin, Russian Far East Liu, Kai The subduction of the Paleo-Pacific oceanic plate in NE China was probably initiated ca. 250 Ma ago. The Mudanjiang Ocean was closed between the Late Jurassic and Early Cretaceous. After that, the roll-back of the Paleo-Pacific oceanic plate and large-scale sinistral strike-slip faulting dominated the tectonics of the NE Asian continental margin. During the early Cenozoic, subduction of the Izanagi-Pacific ridge was subducted extended from SW Japan to Sikhote-Alin. 2021 Thesis http://hdl.handle.net/20.500.11937/84145 Curtin University fulltext |
| spellingShingle | Liu, Kai The subduction history of the Paleo-Pacific Oceanic plate from the Mesozoic to early Cenozoic in NE China and Sikhote-Alin, Russian Far East |
| title | The subduction history of the Paleo-Pacific Oceanic plate from the Mesozoic to early Cenozoic in NE China and Sikhote-Alin, Russian Far East |
| title_full | The subduction history of the Paleo-Pacific Oceanic plate from the Mesozoic to early Cenozoic in NE China and Sikhote-Alin, Russian Far East |
| title_fullStr | The subduction history of the Paleo-Pacific Oceanic plate from the Mesozoic to early Cenozoic in NE China and Sikhote-Alin, Russian Far East |
| title_full_unstemmed | The subduction history of the Paleo-Pacific Oceanic plate from the Mesozoic to early Cenozoic in NE China and Sikhote-Alin, Russian Far East |
| title_short | The subduction history of the Paleo-Pacific Oceanic plate from the Mesozoic to early Cenozoic in NE China and Sikhote-Alin, Russian Far East |
| title_sort | subduction history of the paleo-pacific oceanic plate from the mesozoic to early cenozoic in ne china and sikhote-alin, russian far east |
| url | http://hdl.handle.net/20.500.11937/84145 |