The uplift mechanism and deep crustal deformation of the northeast of the Tibetan plateau in
response to the Cenozoic India-Asian collision are still poorly constrained. Previous studies
linked the uplift mechanism of the northeast of Tibet to the southward underthrusting of the
Asian mantle lithosphere and the northward subduction of the Indian plate; yet, the details of
crustal properties and thickening mechanism beneath the northeast of Tibet remain
controversial. To shed light on the uplift mechanism of the northeast of the Tibetan plateau …