SHRIMP zircon U-Pb geochronological and whole-rock geochemical evidence for an early Neoproterozoic Sibaoan magmatic arc along the southeastern margin of the Yangtze Block
It has been generally accepted that the South China Block was formed through amalgamation of the Yangtze and Cathaysia Blocks during the Proterozoic Sibaoan orogenesis, but the timing and kinematics of the Sibao orogeny are still not well constrained. We report here SHRIMP U–Pb zircon geochronologic...
| Main Authors: | , , , , |
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| Format: | Journal Article |
| Published: |
International Association for Gondwana Research
2007
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/15529 |