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- W1915021902 abstract "[1] We use data from campaign and continuous GPS sites in southeast and south central Alaska to constrain a regional tectonic block model for the St. Elias orogen. Active tectonic deformation in the orogen is dominated by the effects of the collision of the Yakutat block with southern Alaska. Our results indicate that ~37 mm/yr of convergence is accommodated along a relatively narrow belt of N-NW dipping thrust faults in the eastern half of the orogen, with the present-day deformation front running through Icy Bay and beneath the Malaspina Glacier. Near the Bering Glacier, the collisional thrust fault regime transitions into a broad, northwest dipping decollement as the Yakutat block basement begins to subduct beneath the counterclockwise rotating Elias block. The location of this transition aligns with the Gulf of Alaska shear zone, implying that the Pacific plate is fragmenting in response to the Yakutat collision. Our model indicates that the Bering Glacier region is undergoing internal deformation and could correspond to the final stage of offscraping and accretion of sediments from the Yakutat block prior to subduction. Predicted block motions at the western edge of the orogen suggest that the crust is laterally escaping along the Aleutian fore arc." @default.
- W1915021902 created "2016-06-24" @default.
- W1915021902 creator A5032487736 @default.
- W1915021902 creator A5035944435 @default.
- W1915021902 creator A5073557562 @default.
- W1915021902 date "2013-10-01" @default.
- W1915021902 modified "2023-10-18" @default.
- W1915021902 title "Active tectonics of the St. Elias orogen, Alaska, observed with GPS measurements" @default.
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- W1915021902 doi "https://doi.org/10.1002/jgrb.50341" @default.
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