The Bell Springs Formation: Characterization and Correlationof Upper Triassic Strata in Northeast Utah
Upper Triassic strata that lie between the Chinle Formation and Nugget Sandstone along the south flank of the Uinta Mountains in northeastern Utah are distinctive. In the past, these rocks have been lumped together with the overlying or underlying units. These strata are equivalent to the Bell Sprin...
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| Format: | Others |
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BYU ScholarsArchive
2014
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| Online Access: | https://scholarsarchive.byu.edu/etd/5539 https://scholarsarchive.byu.edu/cgi/viewcontent.cgi?article=6538&context=etd |