The vast eastern-Tethyan oceanic domain that throughout the Mesozoic extended between
Gondwana and Eurasia was a puzzle of larger and smaller microcontinents separated by …

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

Integration of lithostratigraphic, magmatic, and metamorphic data from the Lhasa–Qiangtang
collision zone in central Tibet (including the Bangong suture zone and adjacent regions of …

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 Lhasa Terrane in southern Tibet has long been accepted as the last geological block
accreted to Eurasia before its collision with the northward drifting Indian continent in the …

Recent studies of the northeastern part of the Tibetan Plateau have called attention to two
emerging views of how the Tibetan Plateau has grown. First, deformation in northern Tibet …

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

The uplift of orogenic plateaus has been assumed to be coincident with the fluvial incision of
the gorges that commonly cut plateau margins. The Mekong River, which drains the eastern …

Abstract The Qilian Shan, located along the northeastern margin of the Tibetan Plateau, has
experienced multiple episodes of tectonic deformation, including Neoproterozoic continental …