financially supported by the project of nuclear energy development。
The Bayingobi basin is located in the middle of Central Asia Orogenic Belt,at the intersection of Paleo-Asian Ocean and Tethys Ocean,as well as the junction of multiple tectonic plates.This unique tectonic setting und...
This study is financially supported by the National Natural Science Foundation of China(42072181).
The Pearl River Mouth Basin(PRMB)is one of the most petroliferous basins on the northern margin of the South China Sea.Knowledge of the thermal history of the PRMB is significant for understanding its tectonic evoluti...
funded by the National Natural Science Foundation of China (Nos.42172257,41672199,41421002);MOST Special Fund from the State Key Laboratory of Continental Dynamics,Northwest University;the Foundation of Shaanxi Educational Committee (No.16JK1753)。
The Daba Shan orocline is located at the northeastern margin of the Sichuan Basin and has been inferred as a foreland thrust-fold belt of the Qinling Orogen since the Late Triassic.A complete understanding of rock exh...
supported by the National Natural Science Foundation of China(Nos.42072229,41102131);the Fundamental Research Fund for the Central Universities of China(No.12lgpy22);the Guangdong Natural Science Foundation(No.2021A1515011658);the Science and Technology Program of Guangzhou(No.202002030184);the China Scholarship Council。
Low temperature thermochronology plays a key role in the study of the tectonic evolution of the upper crust.History modeling of apatite fission-track requires the apparent age and the confined track-length distributio...
supported by the National Natural Science Foundation of China (No. 41972153);the Geological Survey Project of China Geological Survey (No. DD20160172);the Science and Technology Department of China National Petroleum Corporation (No. 2018A-0104)。
Mesozoic intracontinental orogeny and deformation were widespread within the southern Central Asian Orogenic Belt(CAOB). Chronological constraints remain unclear when assessing the Mesozoic evolution of the central se...
supported by the National Natural Science Foundation of China (Grant Nos. U2006201 & 41930424);the Science and Technology Planning Project of Guangdong Province, China (Grant No. 2020B1212060055)。
The Jiaojia giant gold deposit is the largest gold deposit in China, with a total gold reserve of approximately 1200 t.Until now, the knowledge of the exhumation history of post-mineralization period is limited, in pa...
the National Natural Science Foundation of China(Nos.41702208,41972223);the China Geological Survey(Nos.1212011121261,DD20179607,DD20160060,12120114042801)。
It is still controversial how the high elevation of the Tibetan Plateau established after the Indian-Asian collision during the Cenozoic. The timing of Gangdese magmatic arc exhumation and uplift history would provide...
provided by MIUR(Italian Ministry of University and Research)PRIN funds;the University of Bologna RFO funds
Apatite fission-track analysis and thermochronologic statistical modeling of Precambrian-Oligocenc plutonic and metamorphic rocks from the Lesser Caucasus resolve two discrete cooling episodes.Cooling occurred during ...
supported by the National Natural Science Foundation of China(Grants No.41572102,41330315,41102067,and 41172127);Natural Science Foundation of Shaanxi Province(Grant No.2018JM4001)
Multi-dating on the same detrital grains allows for determining multiple different geo-thermochronological ages simultaneously and thus could provide more details about regional tectonics.In this paper,we carried out ...
funded by the Natural Science Foundation of China (Grants No. 41501209 and 41571177);the Fundamental Research Funds for the Central Universities (862457, lzujbky-2016-22)
The Northern Qaidam Basin is located at the northeastern part of the Qinghai-Tibetan Plateau. It contains very thick Cenozoic terrestrial clastic sediments, which records the formation of the northern Qaidam Basin due...