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|Forsyth Deployment near the South Shatsky Fracture Zone (PLATE)
Two arrays of 8 instruments each designed to study the lithosphere and asthenosphere structure beneath some of the oldest seafloor in the western Pacific. Ocean bottom seismometers deployed for one year in a passive experiment. We will be using surface wave tomography, shear wave splitting, and receiver function analysis to model the upper mantle structure.
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