Provenance of the Chugach-Prince William terrane through U/Pb dating of detrital zircons, Baranof Island, SE Alaska
The southern Alaska continental margin contains the Chugach-Prince William Terrane (CPW), a ~2200 km Mesozoic-Tertiary accretionary complex composed mainly of deep-water turbidites and is intruded by 62-47 Ma near trench plutons of the Sanak- Baranof Belt (SBB). Location of the CPW during intrusion...
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Carleton Digital Commons
2014
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Online Access: | https://digitalcommons.carleton.edu/comps/794 |