Recent studies of the northeastern part of the Tibetan Plateau have called attention to two
emerging views of how the Tibetan Plateau has grown. First, deformation in northern Tibet …

Debate continues over whether global cooling or uplift of the Tibetan Plateau provided the
first-order driver for the aridification (moisture levels) of Central Asia throughout the Mid …

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 Qinling Mountains stretching from east to west in Central China are an
important geological and geographical boundary in the China Continent and even the East …

Abstract The Shanxi Rift System (SRS) is a prominent intracontinental rift in eastern Eurasia.
However, its tectonic origin remains enigmatic, as the timing of rift initiation and its …

Abstract Sedimentary rocks in Tibetan Plateau basins archive the spatiotemporal patterns of
deformation, erosion, and associated climate change that resulted from Cenozoic …

The development of high topography associated with the Indo-Asian collision plays a central
role in ongoing debates over the linkages between development of the Tibetan Plateau and …

Abstract The northeastern Tibetan Plateau occupies the northernmost portion of the plateau,
whose timing and pattern of deformation during its Cenozoic tectonic development provide …

The three-dimensional present-day crustal deformation and strain partitioning in
northeastern Tibetan Plateau are analyzed using available GPS and precise leveling data …

The time-space patterns of deformation throughout the Indo-Asian collision zone can place
constraints on the processes responsible for the development of high topography. Although …