supported by the National Natural Science Foundation of China (Grant Nos.41972190,42302344).
The Xiuyan impact crater is the only officially recognized impact crater in China, and its formation time remains unclear. In this study, we investigated the ages of Xiuyan impact crater lake sediments from a 99-m com...
financed from the statutory funds of the Polish Geological Institute-National Research Institute(projects No. 61.2201.0605.00.0 and No.62.9012.2034.00.0)。
Lower Buntsandstein small—scale cycles recognized in the Central European Basin(CEB) are readily used for astrochronological calibration of the Early Triassic time scales,although they are not well studied sedimentol...
financially supported by the National Natural Science Foundation of China(Grant nos.41941004,42172068,42261144673);the Fundamental Research Funds of the Chinese Academy of Geological Sciences(CAGS)(Grant no.JKYZD202321);Geological Survey Programme(Grant no.DD20221810).
The Prydz Belt in East Antarctica underwent extensive reworking during the late Neoprotertozoic–early Paleozoic Pan-African orogeny,which is characterized by granulite facies,clockwise P–T paths,and high dT/dP value...
supported by the Basic Scientific Fund for National Public Research Institutes of China(Grant No.2023S02);the National Natural Science Foundation of China(Grant Nos.42076076&42376075);the Taishan Scholar Program of Shandong Province。
Oceanic intraplate volcanoes with linear age progressions are usually accepted to be derived from melting of an upwelling mantle plume.Several seamount groups in NW Pacific,however,show complex age-distance relationsh...
financially supported by the China Geological Survey Scientific Research Project(Grant Nos.DD20190167 and DD20190053);the National Natural Science Foundation of China(Grant No.42172259).
The Jitang metamorphic complex is key to studying the tectonic evolution of the Northern Lancangjiang zone.Through structural-lithological mapping,structural analysis and laboratory testing,the composition of the Jita...
funded by the projects of China Geological Survey(Grant Nos.12120113089600,1212011085472,and 12120114028701)。
The southwestern Fujian depression belt(SFDB)is an economically important Mesozoic Fe metallogenic belt in South China and is renowned for its Makeng-type Fe deposits,in which stratified skarn Fe orebodies generally o...
supported by the Australian Research Council(FL160100168)。
The assessment of detrital zircon age records is a key method in basin analysis,but it is prone to several biases that may compromise accurate sedimentary provenance investigations.High to ultrahigh temperature(HT-UHT...
supported by the Deep Resources Exploration and Mining Project(Grant No.2019YFC0605202);China Geological Survey Project(Grant Nos.DD20221684,DD20221795,DD20201173)。
The Nanyuan Formation contains information related to the Mesozoic tectonic transformation.In this study,three representative profiles were surveyed from the Nanyuan Formation,and multiple analyses were conducted.Zirc...
financially supported by the GACR EXPRO Project 19-27682X to K.S.and O.L.;the National Natural Science Foundation of China(41888101)to W.X.;the International Partnership Program of Chinese Academy of Sciences(CAS)(132744KYSB20190039);IGCP 622(CAS)。
The Central Asian Orogenic Belt constitutes the Kazakhstan and Mongolian oroclinal collages located between the Tarim-North China collage(TNC)to the south and the Siberian craton to the north(Fig.1a)[1].While the oroc...
supported by the National Natural Science Foundation of China(Grant No.41872219);the Key Research and Development Program of Shaanxi(Grant No.2019SF-245);the Natural Science Foundation of Shaanxi Province(Grant No.2023-JC-YB-222);an integrated research project of Integrated Exploration of China Geological Survey(Grant No.WKZB1911BJM300369/002)。
The Xiejiaba and Fuqiangbei plutons form part of the newly identified Neoproterozoic Niushan complex,which is located in the southern South Qinling belt(SQB).The plutons are compositionally similar,were emplaced at 75...