U-Pb dating of detrital zircon from turbidites of the Chugach and Prince William terranes, Alaska: Implications for the significance of the Contact fault system as a terrane boundary
The Contact fault system has traditionally been viewed as the terrane boundary between the Chugach and Prince William terranes in southern Alaska. It is thought to divide the Campanian-Maastrichtian Valdez Group from the Paleocene-Eocene Orca Group in an arcuate trace across Prince William Sound (PW...
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Carleton Digital Commons
2019
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Online Access: | https://digitalcommons.carleton.edu/comps/2412 |