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Deformation between the highly oblique Yakutat–North American plate boundary and the Eastern Denali fault
This study investigates the spatial and temporal pattern of rock exhumation inboard of the highly oblique Yakutat–North American plate boundary. We aim to quantify how far deformation is transferred inboard of the Fairweather transform plate boundary and across the Eastern Denali fault. We present new detrital apatite and zircon fission track data from 27 modern drainages collected on both sides of the Eastern Denali fault and from the Alsek and Tatshenshini River catchments that drain thedoi:10.1130/ges02410.1 fatcat:u7ze367lencingpaq3nemmkk7a