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The fate of subducted sediments: A case for backarc intrusion and underplating
GEOLOGY, no. 12 (2007): 1111-1114
Abstract
Subduction of oceanic and continental sediments into the mantle is fundamental to the geochemical evolution of Earth. Using thermal-mechanical models, we examine the dynamics of sediments that are subducted below continental lithosphere. Owing to their low density relative to the mantle, model sediments detach from the subducting plate at...More
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