The often-used phrase 'the uplift of the Tibetan Plateau'implies a flat-surfaced Tibet rose as a
coherent entity, and that uplift was driven entirely by the collision and northward movement …

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 …

Knowledge of the topographic evolution of the Tibetan Plateau is essential for
understanding its construction and its influences on climate, environment, and biodiversity …

The East Asian monsoon plays an integral role in human society, yet its geological history
and controlling processes are poorly understood. Using a general circulation model and …

Tibet's ancient topography and its role in climatic and biotic evolution remain speculative
due to a paucity of quantitative surface-height measurements through time and space, and …

Paleoelevation reconstruction using oxygen isotopes is making a significant contribution to
understanding the Cenozoic uplift of the Himalayas and the Tibetan Plateau. This paper …

Long-standing problems in the geological evolution of the Tibetan–Himalayan orogen
include where the India–Asia convergence was accommodated and how the plateau grew …

The biodiversity of the Himalaya, Hengduan Mountains and Tibet, here collectively termed
the Tibetan Region, is exceptional in a global context. To contextualize and understand the …

Uplift of the Himalaya and Tibetan Plateau (HTP) and its linkage with the evolution of the
Asian monsoon has been regarded as a typical example of a tectonic–climate linkage …