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Figure F2. A portion of depth-corrected seismic Line HD33B through Site C0019. The section is partially interpreted, identifying the reflector at the top of the oceanic igneous crust of the incoming Pacific plate, top of the bedded chert, and sedimentary cover. The location of the reflector interpreted as the main décollement between the subducting Pacific plate and the deformed sediments of the overthrust frontal prism are also shown. VE = vertical exaggeration. Modified from Center for Deep Earth Exploration (2012).

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