Despite a long research history over the past 150 years, the geometry, kinematics, and
dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …

The initial collision between Indian and Asian continents marked the starting point for
transformation of land-sea thermal contrast, uplift of the Tibet-Himalaya orogen, and climate …

Asia has been a major testing ground for various competing models of continental
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …

Abstract The India-Asia collision is an outstanding smoking gun in the study of continental
collision dynamics. How and when the continental collision occurred remains a long …

Timing of the collision between India and Asia is the key boundary condition in all models for
the evolution of the Himalaya‐Tibetan orogenic system. Thus it profoundly affects the …

Although most data suggest that the India–Eurasia continental collision began∼ 45–55 Myr
ago, the architecture of the Himalayan–Tibetan orogen is dominated by deformational …

Reconstructing the evolution of the Bangong-Nujiang Tethyan Ocean (BNTO) plays an
indispensable role in understanding the linkage between Gondwana dispersion and Tibetan …

The time of initial collision between India and Asia has been extremely controversial despite
the fact that it is vital to constraining the orogenesis and subsequent evolution of the …

The northernmost exposures of sub-Himalayan Cenozoic strata in the Hazara–Kashmir
syntaxial region of north Pakistan comprises the Paleocene–Eocene marine strata in the …

The sediment archive, of material eroded from an active tectonic region and stored in
adjacent basins, can provide a valuable record of hinterland tectonism especially when …