The surface uplift history of the Tibetan Plateau (TP) offers a key testing ground for
evaluating models of collisional tectonics and holds important implications for processes …

The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …

Origins of an alpine flora The evolution of high mountain floras is strongly influenced by
tectonic and climatic history. Ding et al. document the timing, tempo, and mode by which the …

The large Gangdese metallogenic belt, located in the southern part of the Tibetan Plateau,
hosts a variety of magmatic-hydrothermal ore deposits. Previous works in the area primarily …

To understand the magmatic and tectonic events in the Eastern Kunlun Range, we
conducted systematic zircon U–Pb geochronology, and paired zircon (ZHe) and apatite …

Exhumation of the southern Tibetan plateau margin reflects interplay between surface and
lithospheric dynamics within the Himalaya–Tibet orogen. We report thermochronometric …

The **gaze forearc basin records the evolution of the southern Lhasa terrane convergent
margin, largely affected by Neo-Tethyan subduction processes, prior to the Paleocene …

Abstract The Tibetan Plateau geographically contains internal and external drainage areas
based on the distributions of river flows and catchments. The internal and external drainage …

Abstract The India-Asia collision zone in southern Tibet preserves a record of geodynamic
and erosional processes following intercontinental collision. Apatite fission-track and zircon …

A complete thermal history for the Qulong porphyry Cu–Mo deposit, Tibet is presented.
Zircon U–Pb geochronology indicates that the mineralization at Qulong resulted from …