Amalgamation between the Yangtze and Cathaysia Blocks in South China: Constraints from SHRIMP U-Pb zircon ages, geochemistry and Nd-Hf isotopes of the Shuangxiwu volcanic rocks
South China was formed through the amalgamation of the Yangtze Block with the Cathaysia Block, but the timing of this amalgamation is controversial, ranging from Mesoproterozoic to Mesozoic. We report here SHRIMP U-Pb zircon ages, geochemistry and Nd-Hf isotopes of the Shuangxiwu Group volcanic rock...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2009
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/7922 |