Clastic wedge development and sediment budget in a source-to-sink transect (Late Campanian western interior basin, SW Wyoming and N Colorado)
The problem of how sand and mud was distributed downslope, within linked alluvial-brackish water-marine shoreline systems of an extensive clastic wedge is addressed here. The Iles Clastic wedge accumulated over a time period of a few million years (my), and its component high-frequency regressive-tr...
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Format: | Others |
Language: | English |
Published: |
2010
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Online Access: | http://hdl.handle.net/2152/7677 |