Provenance history of the Bangemall Supergroup and implications for the Mesoproterozoic paleogeography of the West Australian Craton.
The 4-10 km-thick Bangemall Supergroup, comprising the Edmund and Collier Groups, was deposited between 1620 and 1070 Ma in response to intracratonic extensional reactivation of the Paleoproterozoic compressional Capricorn Orogen. The supergroup can be further divided into six depositional packages...
| Main Authors: | , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2008
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/8901 |