A temporal link between the Emeishan large Igneous Province (SW China) and the end-Guadalupian mass extinction
Previous studies have suggested that there were two mass extinction events in the Late Permian: one that occurred at the Permo-Triassic (P/T) boundary (251 Ma) and a second, smaller mass extinction that occurred 5 8 Myr earlier at the end of the Guadalupian. Many workers have argued that there is a...
| Main Authors: | , , , , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2002
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/44553 |