Abstract
Thermobarometric data from amphibolite-facies metamorphic rocks west of the Coast Mountain Batholith provide important constraints on the structural evolution of the mid-Cretaceous Sumdum-Fanshaw fault system and Late Cretaceous-Paleocene Le Conte Bay shear zone in central southeastern Alaska. -from Authors
Original language | English (US) |
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Pages (from-to) | 912-928 |
Number of pages | 17 |
Journal | Canadian Journal of Earth Sciences |
Volume | 28 |
Issue number | 6 |
DOIs | |
State | Published - 1991 |
ASJC Scopus subject areas
- General Earth and Planetary Sciences