Crustal deformation

Crustal Structures in the SE Tibet

Moho depth and crustal deformation in the SE Tibet

Sharp lateral Moho variations across the SE Tibetan margin and their implications for plateau growth

The tectonic uplift of the Tibetan Plateau is a focus in the geosciences. Mid‐lower crustal flow is a popular model to interpret the geodynamic mechanism on the margin of the Tibetan Plateau. The model predicts different surface and Moho topographies …