Fluvial, shoreline, and clastic wedge responses to foreland basin and Laramide style subsidence: Examples from experimental studies and the Greater Green River Basin, southern Wyoming
Subsidence is one of the main factors controlling the stratigraphy and overall stratal architecture in tectonically active basins. This was particularly important in the Western US Cordilleran foreland and Laramide basins when some other controls were minor, e.g. reduced eustatic fluctuations in the...
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| Format: | Others |
| Language: | en |
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2014
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| Online Access: | http://hdl.handle.net/2152/26608 |