The subduction history of the Paleo-Pacific Oceanic plate from the Mesozoic to early Cenozoic in NE China and Sikhote-Alin, Russian Far East
| dc.contributor.author | Liu, Kai | |
| dc.contributor.supervisor | Simon Wilde | en_US |
| dc.contributor.supervisor | Birger Rasmussen | en_US |
| dc.date.accessioned | 2021-06-21T01:11:05Z | |
| dc.date.available | 2021-06-21T01:11:05Z | |
| dc.date.issued | 2021 | en_US |
| dc.identifier.uri | http://hdl.handle.net/20.500.11937/84145 | |
| dc.description.abstract |
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. | en_US |
| dc.publisher | Curtin University | en_US |
| dc.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 | en_US |
| dc.type | Thesis | en_US |
| dcterms.educationLevel | PhD | en_US |
| curtin.department | School of Earth and Planetary Sciences | en_US |
| curtin.accessStatus | Open access | en_US |
| curtin.faculty | Science and Engineering | en_US |