Tectonic Evolution of the Chugach-Prince William Terrane: Geochemistry of the Orca Group Volcanic Rocks in Eastern Prince William Sound, Alaska

Geologic evidence indicates that slab window subduction modified the forearc basin in the Chugach-Prince William terrane (CPW), producing marine basalts interbedded and structurally interleaved with the Paleocene flysch of the CPW. A similar model is proposed for the nearly coeval Crescent Formation...

Full description

Bibliographic Details
Main Authors: Fryer, Karen H., Young, Elaine K., Davidson, Cameron, Garver, John I.
Format: Text
Language:unknown
Published: Digital Commons @ OWU 2015
Subjects:
Online Access:https://digitalcommons.owu.edu/geol_geog_pubs/4