Abstract
Indicates that the Echo Canyon was derived from three separate stratigraphic sections exposed on the inactive Willard thrust sheet and the eastern flank of the Wasatch basement culmination. -from Author
Original language | English (US) |
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Pages (from-to) | 1039-1043 |
Number of pages | 5 |
Journal | Geology |
Volume | 16 |
Issue number | 11 |
DOIs | |
State | Published - 1988 |
ASJC Scopus subject areas
- Geology