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 |
|---|---|
| Pages (from-to) | 71-95 |
| Number of pages | 25 |
| Journal | Utah Geol & Mineralogical Survey-Bul 82 |
| Publication status | Published - May 1969 |
| Externally published | Yes |