The Sanjiang region in SE Tibet Plateau, and the western Yunnan region in southwestern
China constitute a collage of Gondwana-derived micro-continental blocks and arc terranes …

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 …

This paper reviews the tectonic, magmatic, and metallogenic history of the Tethyan orogen
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …

The Asian continent consists of many continental blocks that assembled during the
Phanerozoic, accompanied by widespread granitoids. By compiling a series of digital maps …

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 …

Within the Himalayan collisional belt, granotoids occur along two sub-parallel belts, the
Northern Himalayan Gneiss Domes (NHGD) and the High Himalayan Crystalline Series …

Ultrapotassic lavas having distinct geochemical compositions (K2O/Na2O> 2, K2O> 3%, and
MgO> 3%) are common and widespread on the Tibet Plateau, where they are closely linked …

Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

As a crucial part of the Asian monsoon stretching from tropical India to temperate East Asia,
the Indian monsoon (IM) contributes predominant precipitation over Asian continent …

The Central Asian Orogenic Belt (CAOB) is a natural laboratory for the study of accretionary
tectonics and crustal growth owing to its massive generation of juvenile crust in the …