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<正>Objective The lateral extrusion of crustal materials around the southeastern edge of the Tibetan Plateau since the Oligocene is believed to be one of the main inducements of~1300 km latitudinal crustal convergence in the Tibetan Plateau,since the collision of India and Eurasia in the Paleogene.Two end-member models were used to describe the process of lateral extrusion of crustal material 相似文献