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...
Main Authors: | , , , |
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Format: | Text |
Language: | unknown |
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Digital Commons @ OWU
2015
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Online Access: | https://digitalcommons.owu.edu/geol_geog_pubs/4 |