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The garnet placer deposit preserves a record of the complete rock pattern, operative on less then 10-My geologic timescales, including subduction of sedimentary protoliths to UHP circumstances, fast exhumation, area uplift, and erosion. Detrital garnet geochemistry and addition rooms from both contemporary sediments and stratigraphic areas could be used to decipher the petrologic evolution of plate boundary areas and present recycling processes throughout Earth's hist