the National Natural Science Foundation of China(Grant Nos.42230308,42072266,42102032,42362006);Bureau of Geological Exploration and Development of Qinghai Province(Grant Nos.[2023]33,[2022]32);China Geological Survey(Grant Nos.DD20221649,DD20242935,12120114079701).
Fragments of Proto-Tethyan oceanic lithosphere are well-preserved along the southern belt of the North Qilian suture,and the origin and emplacement of these ophiolites have become subjects of intense debate.In this st...
jointly supported by the National Natural Science Foundation of China(Grant Nos.42202077,42473029);the Natural Science Foundation of Gansu Province(Grant Nos.22JR5RA440,20JR10RA630);the Fundamental Research Funds for the Central Universities(Grant No.LZUJBKY-2022-42);the Guiding Special Funds of“Double First-Class(First-Class University&First-Class Disciplines)”of Lanzhou University,China(Grant No.561119201)。
The study of metallogeny includes origin,development,modification,and preservation of mineralisation.The understanding of temporal evolution,and post-mineralisation modification and preservation of mineralisation are ...
financially supported by the National Natural Science Foundation of China(Grant Nos.42172258,42072227,U2244205);the Science and Technology Major Project of Xinjiang Uygur Autonomous Region,China(2023A03002);the National Key Technology Research and Development Program of the Ministry of Science and Technology of China(Grant No.2015BAB05B04);the Joint Innovation Fund of China National Uranium Co.,Ltd.,and State Key Laboratory of Nuclear Resources and Environment(Grant No.NRE2021-01);the China Geological Survey(Grant Nos.DD20242868,DZLXJK202206)。
The Southwest Tianshan is the suture zone between the Central Tianshan and the Tarim Craton.To better illustrate the subduction polarity of the Southwest Tianshan Ocean,a systematic detrital zircon LA-ICP-MS U-Pb geoc...
financially supported by the Basic Foundation of Tianjin University of Commerce;the Fund from the Key Laboratory of Continental Dynamics of Ministry of Natural Resources(J2306)。
Deciphering high-pressure granulite-facies metamorphism and anatexis within a collisional orogeny can provide crucial constraints on geodynamic evolution and melt activity during subduction and exhumation.Combining pe...
financially supported by the Fundamental Scientific Research Project of Institute of Geology,China Earthquake Administration(Grant No.IGCEA2016);the National Natural Science Foundation of China(Grant Nos.42204072 and 41804055);the National Key Research and Development Program of China(Grant No.2017YFC1500103)。
The Ordos Block,the western part of the North China Craton(NCC),has preserved most of its cratonic lithospheric roots during the destruction and modification of the NCC,and nowconnects two distinctly different tectoni...
supported by the National Natural Science Foundation of China grant(U2244220);China Geological Survey Project grant(DD20190551,DD20230351)。
The Qilian Orogenic belt is one of the typical orogenic belts globally and a natural laboratory for studying plate tectonics.Many researchers have studied the ophiolite and high pressure and ultra-high pressure metamo...
financially and technically supported by the University of Birjand under Project Number 7912.
The eastern Iranian range,known as the Sistan suture zone in the past,has recently been identified as the Sistan orogen.This Paleogene orogeny is located between the Lut and Afghan microcontinents.The structural analy...
supported by Records of China’s Mineral Geology from the China Geological Survey(DD20190379);the State Key Program of National Natural Science Foundation of China(41730426);the 111 Project of the Ministry of Science and Technology(BP0719021)。
1.Objective The West Qinling Orogen extends east-west over 1500 km and is endowed with dozens of large-super large scale gold deposits.The Zaozigou gold deposit has a proven reserve of 134 t with an average grade of 3...
supported by the Opening Fund of Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes(No.Y840041117);the National Natural Science Foundation of China(No.42102199).
Abundant mafic-felsic intrusions distributed in the Altyn Orogen record orogenic histories related to Proto-Tethys and Paleo-Tethys evolution.Zircon U-Pb dating of the intrusive rocks in the eastern Altyn Orogen ident...
financially supported by the State Key Research Development Program of China(Grant No.2022YFF0800903);the National Natural Science Foundation of China(NSFC)(Grant Nos.42261144669 and 42273073)。
High-silica granitoids record the formation and evolution of the continental crust.A new intrusive complex has been recognized among silicic volcanic rocks of the Weixi arc,Southwest China.The intrusions consist of gr...