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 |
|---|---|
| Pages (from-to) | 912-928 |
| Number of pages | 17 |
| Journal | Canadian Journal of Earth Sciences |
| Volume | 28 |
| Issue number | 6 |
| DOIs | |
| State | Published - 1991 |
| Externally published | Yes |
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