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|Deep Structure of the Nortwaster Tibet Collison Zone (INDEPTH4)
An extension of INDEPTH 3. Testing hypotheses for the uplift of north Tibet. 1. imbricating of Asian crust while the Asian continental lithosphere is being detached and "subducted" into the Tibetan mantle; 2. delaminating of a thickened Tibetan lithosphere and 3. asthenospheric counter flow associated with subduction of Indian continental lithosphere
|Digital Object Identifier (DOI)
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