Rodinian devil in disguise: Correlation of 1.25-1.10 Ga strata between Tasmania and Grand Canyon
Locating the continuation of the ca. 1.30-1.00 Ga Grenville orogen on continents formerly adjacent to Laurentia is central to resolving the paleogeography of the supercontinent Rodinia. Here we emphasize a correlation of late Mesoproterozoic foreland basins that, prior to truncation by Neoproterozoi...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Geological Society of America
2018
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| Online Access: | http://hdl.handle.net/20.500.11937/72302 |