An increasing number of detrital zircon U–Pb geochronological data have been reported to
trace sediment provenance for the Cenozoic Qaidam basin, which is crucial to …

Quaternary aeolian silts in the Chinese Loess Plateau (CLP) has long been regarded as a
product of sand ablation during the process of transportation originally from sandy deserts of …

柴达木盆地厚达万米的新生代沉积物记录了青藏高原东北部隆升和古气候变化信息.
本文基于盆地北缘大红沟剖面高分辨率的磁极性年代标尺, 对该剖面古‒新近纪河湖相沉积物 …

Chemical weathering of continental silicates is a crucial geological process in regulating
Earth's long-term climate and participating in global carbon cycle. The increasing aridity and …

Sedimentary rocks in northern Tibet record uplift of the Tibetan Plateau and its potential
connection with the evolution of the central Asian aridity, therefore offering a typical example …

Abstract The Tibetan Plateau was built through a succession of Gondwanan terranes
colliding with Asia during the Mesozoic. These accretions produced a complex Paleogene …

Unravelling early Cenozoic basin development in northern Tibetan Plateau remains crucial
to understanding continental deformation mechanisms and to assessing models of plateau …

The evolution of the tectonic deformation of the northeastern Tibetan Plateau (TP) in the
Cenozoic is significant for understanding plateau growth during India‐Asia convergence …

Sediment source-to-sink history is pivotal to investigating the evolution of ancient
sedimentary basin. Previous study focuses mostly on reconstruction of various components …

The formation of high topography on the northeastern margin of the Tibetan Plateau (the
Qilian Shan) constrains the evolutionary history of the plateau. Although prominent …