Variable involvements of mantle plumes in the genesis of mid-Neoproterozoic basaltic rocks in South China: A review
Ca. 825-720 Ma global continental intraplate magmatism is generally linked to mantle plumes or a mantle superplume that caused rifting and fragmentation of the supercontinent Rodinia. Widespread Neoproterozoic igneous rocks in South China are dated at ca. 825-760 Ma. There is a hot debate on their p...
| 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/20.500.11937/7034 |