Abstract The Tibetan Plateau (TP) impacts local and remote atmospheric circulations,
wherein it mechanically and thermally affects air masses or airflows. Moreover, the TP …

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 …

Using data from more than 2000 seismic stations from multiple networks arrayed throughout
China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean …

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 …

Chemical geodynamics is an integrated discipline that studies the geochemical structure
and tectonic evolution of geospheres with the aim of linking tectonic processes to …

Convective removal of lower lithosphere beneath the Tibetan Plateau can account for a
rapid increase in the mean elevation of the Tibetan Plateau of 1000 m or more in a few …

Field observations and satellite geodesy indicate that little crustal shortening has occurred
along the central to southern margin of the eastern Tibetan plateau since about 4 million …

Thermochronologic, sedimentologic, oceanographic, and paleoclimatic studies suggest that
rapid uplift and unroofing of southern Tibet began about 20 million years ago and that the …

The Tibetan Plateau, between the Kunlun Shan and the Himalayas, consists of terranes
accreted successively to Eurasia. The northernmost, the Songban Ganzi Terrane, was …

Following an Eocene continent-arc collision, the Western Anatolia region experienced a
complete cycle of thickening and orogenic collapse. The early stage of collision-related …