Near-Salt Stratal Geometries and Implications for the Evolution of the Onion Creek Diapir Moab, UT
The Onion Creek Diapir is one of many salt domes proximal to the Uncompahgre thrust front of the ancestral rockies in the Paradox Basin. It is comprised of Paradox Formation evaporites and large blocks of Honaker Trail Formation carbonates that were deformed by loading of Permian Cutler Formation pr...
| Main Author: | |
|---|---|
| Format: | Others |
| Published: |
BYU ScholarsArchive
2017
|
| Subjects: | |
| Online Access: | https://scholarsarchive.byu.edu/etd/6327 https://scholarsarchive.byu.edu/cgi/viewcontent.cgi?article=7327&context=etd |