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We combine seismological and Bouguer anomaly data with thermo-kinematic and petrological modelling to constrain the extent and kinetics of the eclogitization process in the Indian lower crust underthrusting Tibet. Based on Airy-type isostasy gravity modelling, we show that the presence of denser material (eclogites) is required beneath the Tibetan Plateau. Using the geometries of main crustal interfaces...
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