R Zhu, P Zhao, L Zhao - Science China Earth Sciences, 2022 - Springer
Abstract The Neo-Tethys Ocean was an eastward-gaping triangular oceanic embayment between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …
How the continental lithosphere deforms far away from plate boundaries has been long debated. The Tianshan is a type-example of ongoing lithospheric deformation in an …
J Deng, Q Wang, G Li, M Santosh - Earth-Science Reviews, 2014 - Elsevier
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 continental crust of China is a mosaic of cratonic blocks and orogenic belts, containing small cratons and terranes with various tectonic settings. They have diverse origins and …
Cenozoic convergence between the Indian and Asian plates produced the archetypical continental collision zone comprising the Himalaya mountain belt and the Tibetan Plateau …
Chemical geodynamics is an integrated discipline that studies the geochemical structure and tectonic evolution of geospheres with the aim of linking tectonic processes to …
The recent discovery of large porphyry copper deposits (PCDs) associated with Miocene (22– 12 Ma) granitoid magmas in the eastern section of the Paleocene-Eocene Gangdese …
X Bao, X Song, J Li - Earth and Planetary Science Letters, 2015 - Elsevier
We present a new high-resolution shear-velocity model of the lithosphere (down to about 160 km) beneath China using Rayleigh-wave tomography. We combined ambient noise and …
J Li, X Song - Proceedings of the National Academy of …, 2018 - National Acad Sciences
What happened to the Indian mantle lithosphere (IML) during the Indian–Eurasian collision and what role it has played on the plateau growth are fundamental questions that remain …