Spatial Trends and Facies Distribution of the High-Energy Alluvial Cutler Formation, Southeastern Utah
The Cutler Formation is composed of thick, arkosic, alluvial conglomerate, sandstone, and mudstone shed southwestward from the Uncompahgre Uplift into the Paradox Basin. More basin-ward the Cutler is recognized as a group consisting of differentiable formations. Discrete formations historically have...
| Main Author: | |
|---|---|
| Format: | Others |
| Published: |
BYU ScholarsArchive
2016
|
| Subjects: | |
| Online Access: | https://scholarsarchive.byu.edu/etd/6253 https://scholarsarchive.byu.edu/cgi/viewcontent.cgi?article=7253&context=etd |