Abstract
Surface sedimentary rocks in northern Utah and adjacent areas are unconformably underlain by granite-gneiss- migmatite complexes of Precambrian age. General review of the geologic evolution of these Precambrian terranes is given based on existing geologic and geochronologic data.
Original language | English |
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Pages (from-to) | 71-95 |
Number of pages | 25 |
Journal | Utah Geol & Mineralogical Survey-Bul 82 |
Publication status | Published - May 1969 |
Externally published | Yes |