The Roles of Far Field Stress and Mantle Downwelling In Intraplate Deformation: The Michigan Basin
The Michigan basin has long been established as the type example of an intracratonic basin due to its near circular geometry and gently inward-dipping Paleozoic formations. The backstripping of major formations within the basin reveals that its geometry varied over the duration of the Paleozoic, dis...
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| Language: | en_ca |
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2012
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| Online Access: | http://hdl.handle.net/1807/33802 |