Microstructures and seismic properties of amphibolites along the southern Ailao Shan–Red River belt: Implications for Oligo-Miocene crustal deformation in the southeastern Tibetan Plateau
The mechanism of Oligo–Miocene crustal deformation in the southeastern Tibetan Plateau has long been debated. The two widely cited models of rigid block extrusion and lower-crustal flow still show significant differences in explaining the rheological properties and deep geodynamic characteristics of the continental cru...