A fluvial record of plate-boundary deformation in the Olympics Mountains
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چکیده
(2) What is driving orogenesis for the Olympic Mountain segment of the Cascadia Subduction Zone? Is it shortening parallel to the direction of plate convergence, shortening normal to the direction of plate convergence, or some combination of both? Are there any geomorphic or stratigraphic field relationships that can actually be used to track the horizontal movement of rocks and thus interpret the shortening history over geologic time scales?
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تاریخ انتشار 2002