Structural relationships and crustal deformation in the Saint Elias Orogen, Alaska

The most recent period of orogenesis in southern Alaska began in late Neogene time with the collision of the Yakutat microplate, which is partially accreted to and partially subducted beneath the Alaskan margin to form the St. Elias Mountains. One of the most dynamic areas within the orogen is the E...

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Bibliographic Details
Main Author: Chapman, James Benjamin
Format: Text
Language:English
Published: ScholarWorks@UTEP 2008
Subjects:
Online Access:https://scholarworks.utep.edu/dissertations/AAI1455875