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...
funded by Natural Science Foundation of China(41572190);National Basic Research Program of Ministry of Science and Technology of the People's Republic of China(2015CB453002);China Geological Survey(121201102000150009-16,12120115069601)
The apatite fission track dating of samples from the Dabashan (i.e., the Langshan in the northeastern Alxa Block) by the laser ablation method and their thermal history modeling of AFT ages are conducted in this stu...
supported by the National Natural Science Foundation of China (grant No.41472101)
This work aims to reconstruct the burial history of various kinds of sandstones penetrated by the well YS201 in the Yaoyingtai region of the Changling Fault Depression, southern Songliao Basin, China. Analyses of flui...
supported by the National Natural Science Foundation of China(grant No.41302159)
Objective The uplift process and uplift mechanism of the Tibetan Plateau has been a research focus among geologists in recent years. This work put emphasis on the Cenozoic exhumation histories of the blocks bounded by...
sponsored by the Science Foundation of China University of Petroleum,Beijing (No. QD-201007);the National Nature Science Foundations of China (Grant No. 41102133);financially supported by the foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (No. PRP/indep-4-1110)
The early stage of Sichuan Basin formation was controlled by the convergence of three major Chinese continental blocks during the Indosinian orogeny that include South China,North China,and Qiangtang blocks.Although t...