co-funded by the National Key Research and Development Project 'Key scientific issues of transformative technology' (Grant No. 2019YFA0708601);the second Tibetan Plateau Scientific Expedition and Research Program (STEP) Grant (Grant No. 2019QZKK0802);the Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (Grant No. GML2019ZD0201);National Natural Science Foundation of China (Grant Nos. 41502198, 40921001, 41672223);Research Grant of Chinese Academy of Geological Sciences (Grant No. J2024);Geological Survey of China (Grant Nos. DD20190057, DD20190060)。
The history and geodynamic mechanisms of Cenozoic exhumation and denudation of the Lhasa terrane(LT),southern Tibetan Plateau, remain poorly constrained. Most previous studies investigating the exhumation of the LT ha...
supported by the National Natural Science Foundation of China(No.40921001 and No.40921001);the Geological Survey of China(No.1212010818094)to Xu;the Natural Sciences and Engineering Research Council of Canada to Ji
Although the Indus-Tsangpo Suture(ITS) is the most spectacular thrust system of continent-continent collision in the world, fundamental questions about its strength evolution and deformation behavior transition remain...
supported by the China Postdoctoral Science Foundation (No.2015M571083, 2016T90122);a Fund from the State Key Laboratory of Continental Tectonics and Dynamics, the National Natural Science Foundation of China (No.40921001);the Geological Survey of China (Nos.1212010818094, 12120114057401);a grant from the Ministry of Land and Resources of China (No.201511022)
Zircon U-Pb geochronology, Hf isotope and whole-rock geochemistry were performed on the tuffs of the Yeba Formation in the Gangdese magmatic belt, South Tibet. The results are used to detail the age, source nature and...