PETROLOGY OF DEEP CRUSTAL XENOLITHS FROM THE EASTERN SNAKE RIVER PLAIN, IDAHO (GEOTHERMOMETRY, PRECAMBRIAN)
Xenoliths, collected from certain hybrid lava flows and vents at three localities in the eastern Snake River Plain region of southern Idaho, were derived from underlying crustal terrains which experienced granulite-facies metamorphism at approximately 3.0 AE. Lithologically, charnockite, opdalite, e...
| Main Author: | |
|---|---|
| Format: | Others |
| Language: | English |
| Published: |
2007
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/1911/15845 |