Subduction and closure of the Proto-Tethys and Palaeo-Tethys oceans were important
events in the assembly of Eurasia, and created the Central China Orogenic Belt (CCOB) …

The recent discovery of numerous large porphyry Cu deposits in the southern Qinghai-Tibet
Plateau shows that porphyry Cu deposits can be hosted in magmatic suites in collisional …

Abstract The Proterozoic–Phanerozoic tectonic evolution of the Qilian Shan, Qaidam Basin,
and Eastern Kunlun Range was key to the construction of the Asian continent, and …

Abstract The Wulonggou Pluton is located in Wulonggou area, eastern segment of the
Eastern Kunlun Orogenic Belt, NW China, and consists of mainly alkali-feldspar granites …

High-K magmatism of the central Urumieh–Dokhtar magmatic arc (UDMA) documents the
final stages of Neo-Tethyan Ocean subduction. The temporal and spatial development of …

Collision-related magmatism in accretionary-to-collisional orogens records a tectonic
transition from early subduction-accretionary processes to collisional orogenesis, and also …

Abstract Although the Cenozoic Indo-Asian collision is largely responsible for the formation
of the Tibetan plateau, the role of pre-Cenozoic structures in controlling the timing and …

Abstract The Longshou Shan of western China is the northern backstop of the Cenozoic
Himalayan-Tibetan orogen and occupies a key linkage between the Tarim continent and …

Abstract The Central and South Pamir tectonic blocks contain scarce Late Cretaceous mafic
and intermediate–silicic igneous rocks that represent typical intraplate magmatism distant …

Abstract The late Early Paleozoic volcanic rocks in the East Kunlun orogen are crucial to
determining collisional processes related to the evolution of the Proto-Tethys Ocean. We …