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 Tianshan range, located in the southern Central Asian Orogenic Belt (CAOB),
represents an excellent natural laboratory for investigating intracontinental deformation. The …

Measurements at∼ 400 campaign‐style GPS points and another 14 continuously recording
stations in central Asia define variations in their velocities both along and across the Kyrgyz …

Eastward transport and clockwise rotation of crust around the southeastern margin of the
Tibetan Plateau dominates active deformation east of the Eastern Himalayan Syntaxis …

The timing of uplift of the Tibet Plateau has a central role in the development of tectonic
models for the Tibet Plateau and Cenozoic global climate change. A detailed …

The Asian interior contains the Central Asian Orogenic Belt (CAOB, the longest accretionary
orogen on Earth), the largest mid-latitude desert, and the most widespread late Cenozoic …

During the Mesozoic, the active southern margin of Eurasia was the site of several accretion
and collision events that fit into a framework of convergence between Eurasia and …

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 …

As a typical intracontinental orogenic belt, the Tian Shan range is a natural lab for the
understanding of ongoing intraplate deformation and related geodynamic mechanisms …

We have carried out a detailed magnetostratigraphic study of Tertiary sediments in the
northern margin of the Qaidam Basin, northern Tibetan plateau. A total of 400 …