Abstract The Central China Orogenic Belt (CCOB) comprises, from the east to the west, the
Tongbai-Dabie, Qinling, Qilian and Kunlun Orogens, and preserves abundant and important …

As the largest depression in the Tibetan plateau, the Qaidam basin preserves over 10 km
thick of Cenozoic sediments. Those sediments represent a unique archive of the evolution of …

Abstract The Qilian Shan, located along the northeastern margin of the Tibetan Plateau, has
experienced multiple episodes of tectonic deformation, including Neoproterozoic continental …

Abstract Sedimentary deposits in Tibetan Basins archive the spatial‐temporal patterns of the
deformation and surface uplift processes that created the area's high topography during the …

The growth of the Tibetan Plateau resulted primarily from India-Asia convergence since
initial collision at 65–55 Ma. The Cenozoic Qilian Shan thrust belt and the left-slip strike …

Abstract The Cenozoic Qilian Shan thrust belt is the northern margin of the Tibetan Plateau,
which developed in part due to progressive India-Asia convergence during Himalayan …

Abstract Uplift of the Tibetan Plateau and the distribution of deformation across it are the
result of India-Asia collision, which bring an opportunity of understanding intracontinental …

Mountains grow upward and outward when the accretion of material outpaces its removal.
Mountain building is synergistically influenced by geodynamics, internal structures (crustal …

Collision-induced continental deformation commonly involves complex interactions between
strike-slip faulting and off-fault deformation, yet this relationship has rarely been quantified …

Marking the northern boundary of the Tibetan plateau, the Altyn Tagh fault plays a crucial
role in accommodating the Cenozoic crustal deformation affecting the plateau. However, its …