Neoproterozoic to Paleozoic long-lived accretionary orogeny in the northern Tarim Craton
The Tarim Craton, located in the center of Asia, was involved in the assembly and breakup of the Rodinia supercontinent during the Neoproterozoic and the subduction-accretion of the Central Asian Orogenic Belt (CAOB) during the Paleozoic. However, its tectonic evolution during these events is contro...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
American Geophysical Union
2014
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| Online Access: | http://hdl.handle.net/20.500.11937/44222 |