Triassic sedimentation and postaccretionary crustal evolution along the Solonker suture zone in Inner Mongolia, China
Detrital zircon U-Pb dating of the Xingfuzhilu Formation in southern Inner Mongolia yields a maximum depositional age of around 220 Ma. The predominantly Permian and Triassic zircons are characterized by oscillatory zoning and euhedral shapes, with mostly positive zircon εHf(t) values (+2.0 to +16.4...
| Main Authors: | , , , , , |
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| Format: | Journal Article |
| Published: |
American Geophysical Union
2014
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| Online Access: | http://hdl.handle.net/20.500.11937/18361 |