The age, extent and nature of the uplift of the Tibetan Plateau are currently hotspots and
difficulties in domestic and foreign research. The Lhasa terrane is located in the central and …

The history and geodynamic mechanisms of Cenozoic exhumation and denudation of the
Lhasa terrane (LT), southern Tibetan Plateau, remain poorly constrained. Most previous …

Four intensive uplift periods, ie, 60-35, 25-17 and 12-8 Ma (but 18-13 Ma in the Himalayas of
the southern Tibet), and since about 5 Ma, can be determined on the Tibetan Plateau by …

The collision of the Indian plate and Eurasian plate in Cenozoic led to the deformation and
uplift of nearly 2000 kilometers north of the Himalayan orogenic belt, forming the Tibetan …

Abstract The Altyn Tagh and Qilian Mountains define the northern boundary of the Tibetan
Plateau. Their uplift-exhumation history in the Cenozoic records the deformation and …

The growth of the Tibetan Plateau governs Asian tectonics, geomorphology, and climate
change in the Cenozoic. The Qilian Shan is a fold-and-thrust belt that defines the …

The tectonogeomorphology is regarded as the key to understanding the uplift history of the
Tibetan Plateau. But its research is blocked by the poor constrains of chronology. The low …

Abstract The Haiyuan-Liupan Shan delimits the northeastern margin of the Tibetan Plateau.
We present the integrated results of new stratigraphic investigations, apatite fission track …

The Himalayan orogen characterized by very high variability in tectonic and climatic
processes, and is thus regarded as a natural laboratory for investigating the coupling of …

The growth pattern of the eastern Tibet is still mysterious, where the remnant upland with low
relief has been hypothesized as the response to lower crustal flow originating from the over …