supported by the Open Project Program of Hebei Province Collaborative Innovation Center for Strategic Critical Mineral Research,Hebei GEO University,China(No.HGUXT-2023-14);the China Geological Survey(DD20221646);National Natural Science Foundation of Hebei Province(Nos.D2020402013 and D2023402022);National Natural Science Foundation of China(No.42102091).
Despite the growing concern regarding post-mineralization thermo-tectonic processes in recent years,the relative roles in exhuming and preserving ore deposits remain highly controversial.This study presents new apatit...
financially supported by the China Geological Survey(No.DD20230213);the National Key Research and Development Project(No.2019YFA0708601);Shanxi Province Natural Science Foundation(No.2020JM-310)。
The Altai-Sayan region,an active intracontinental mountain belt characterized by high relief,has undergone multiple phases of intense mountain building and denudation throughout the Mesozoic and Cenozoic.As this mount...
Intraplate structural deformation is diagnostic of tectonic stress regime changes linked to plate interactions and can result from superposed tectonic events whose single contributions are hardly distinguishable.In th...
the Foundation of State Key Laboratory of Nuclear Resources and Environment(Grant Nos.NRE2021-01,2022NRE34);the National Natural Science Foundation of China(Grant No.42162013);the Third Xinjiang Scientific Expedition Program(Grant No.2022xjkk1301);the Fund of National Key Laboratory of Science and Technology on Remote Sensing Information and imagery Analysis,Beijing Research Institute of Uranium Geology(Grant No.6142A01210405).
Xiazhuang uranium ore field,located in the southern part of the Nanling Metallogenic Belt,is considered one of the largest granite-related U regions in South China.In this paper,we contribute new apatite fission track...
The National Natural Science Foundation of China under contract No.42072181;the CNOOC Research Project"Resource Potential,Reservoir Formation Mechanism and Breakthrough Direction of Potential Oil-rich Depressions in Offshore Basins of China(YXKY-ZX 012021)"。
Significant advancements have been made in the study of Mesozoic granite buried hills in the Songnan Low Uplift(SNLU)of the Qiongdongnan Basin.These findings indicate that the bedrock buried hills in this basin hold g...
funded by the National Natural Science Foundation of China(Nos.41972208,42172251).
The topography of the Harlik Mountain has a strong impact on the formation of current arid climate in the Turpan-Hami Basin.However,it is still controversial if Harlik Mountain experienced significant exhumation durin...
supported by the Major National Science and Technology Projects of China(No.2016ZX05034001-006);the National Natural Science Foundation of China(Nos.42072132,41202104,and 41572131);the China Geological Survey Projects(Nos.DD20190103 and DD20190711)。
The Daqing Shan(DQS)located in the Yinshan-Yanshan Orogenic Belt plays an important role in the Mesozoic to Cenozoic evolution of the North China Craton.However,the cooling and exhumation history since the Cretaceous ...
financially supported by the National Natural Science Foundation of China(Grant Nos.41671011,41871019,41877292,41972212);Research Foundation of Chutian Scholars Program of Hubei Province(Grant No.8210403);Shanxi Key Research and Development program:Feng Cheng(Grant No.2021SF2-03).
Plate subduction leads to complex exhumation processes on continents.The Huangling Massif lies at the northern margin of the South China Block.Whether the Huangling Massif was exhumed as a watershed of the middle reac...
The AraçuaíOrogen,in eastern Brazil,was formed during the Neoproterozoic–Cambrian amalgamation of West Gondwana.During the Mesozoic–Cenozoic opening of the South Atlantic Ocean,and the associated divergent tectonic...
supported by National Key Research and Development Program of China(2022YFC2905001,2018YFC0604105);the Opening Foundation of Ministry of Natural Resources Key Laboratory for Mineral Deposits Research,Chengdu University of Technology(grant number:gzck202104);the Fund for Scientific Research-Flanders(FWO,Bilateral Project VS06520N);China Scholarship Council(201908320260,201806190214);support for W.Su and Z.He for their research stay in Belgium.S.Glorie is supported by an Australian Research Council Future Fellowship(FT210100906)。
The Tibetan Plateau geographically contains internal and external drainage areas based on the distributions of river flows and catchments.The internal and external drainage areas display similar highelevations,while t...