Palinspastic reconstruction and geological evolution of Permian residual marine basins bordering China and Mongolia
One main feature of the tectono-paleogeographic evolution of the southern branch of the Paleo-Asian Ocean was that there developed residual marine basins in former backarc/forearc regions after the disappearance of oceanic crust. The paper illustrates the viewpoint taking the evolution of Dalandzadg...
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| Format: | Article |
| Language: | English |
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SpringerOpen
2014-04-01
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| Series: | Journal of Palaeogeography |
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| Online Access: | http://www.sciencedirect.com/science/article/pii/S2095383615300729 |