Erosion of orogenic mountain ranges exhumes deeply buried rocks and controls
weathering, climate, and sediment production and transport at a variety of scales. Erosion …

Abstract The NNE-trending Linglong Metamorphic Core Complex hosts the majority of the
gold deposits in the Jiaodong Peninsula of eastern China. Many of the deposits are hosted …

The onset of mountain building along margins of the Tibetan Plateau provides a key
constraint on the processes by which the high topography in Eurasia formed. Although …

The appearance of detritus shed from mountain ranges along the northern margin of the
Tibetan Plateau heralds the Cenozoic development of high topography. Current estimates of …

The uplift processes of the Qilian Shan (northern Tibetan Plateau) play a central role in our
understanding of the dynamics of outward and upward growth of Tibet due to sustained …

Abstract The Qilian Shan, at the northeastern frontier of the Tibetan Plateau, is a key area for
studying the expansion mechanism of the Tibetan Plateau. Although previous …

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 Cenozoic Tian Shan is one of the preeminent examples of an intracontinental orogen.
However, there remains a significant controversy over when deformation related to the India …

Detrital studies that utilize zircon U–Pb geochronology and fission-track (FT)
thermochronometry are subject to a range of potential sources of bias that should be …

Unraveling the growth of northern Tibet is crucial to understanding the geodynamic
processes of the India-Eurasia collision, evaluating plateau uplift models and reconstructing …