supported by the National Natural Science Foundation of China(Grant Nos.42372071,41421002);the Foundation for the Author of National Excellent Doctoral Dissertation of China(Grant No.201324);a research grant of the State Key Laboratory of Continental Dynamics(Grant No.SKLCD-04).
Mafic enclaves in granites are generally considered to represent coeval mafic melts that derived from metasomatized mantle,which can provide valuable information about crust-mantle interaction.Exploring the genetic li...
supported by projects from the National Natural Science Foundation of China(No.42002098);the Natural Science Foundation of Hebei Province(No.D2020209017,No.D2022107003);China Basic Scientific Research Business Fund Project of the Chinese Academy of Geological Sciences(No.JKY202016);the Innovation and Entrepreneurship Training Program for College Students(No.X2022118);North China University of Science and Technology.
The Zaozigou gold deposit lies south of the Xiahe-Hezuo regional fault zone in the western Qinling orogenic belt and contains many intermediate to felsic dikes.Diorite porphyry,quartz diorite porphyry and biotite dior...
financially supported by China Geological Survey Project(Grant No.DD20220971)。
Located along the southern part of the West Qinling orogenic belt,the Yangshan gold deposit is one of the largest in China.The major gold ores of Yangshan are disseminated in metasedimentary host rocks with minor nati...
supported by the National Natural Science Foundation of China(Grant Nos.41102037,41421002);the Foundation for the Author of National Excellent Doctoral Dissertation of China(Grant No.201324);research grant of State Key Laboratory of Continental Dynamics(Grant No.SKLCD-04)。
The variations in source rocks and melting conditions of granites can provide essential clues for the crustal magmatic response in orogenic process.Based on geochronology,whole-rock and mineral chemistry,this paper re...
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...
supported financially by the National Nature Sciences Foundation of China (grants No. 41872233, 41872235, 41802234, 41472191, 41502191, 41172186, 40972136);China Geological Survey (grants No. 12120114041201, DD2016007901);China Scholarship Council (grant No. 201806565026);China Postdoctoral Science Foundation (2016M592726);the Fundamental Research Funds for the Central Universities(grants No. 300103183081, 300104282717, 300102279204, 201810710233)
Objective Neocalamites is a common plant fossil from the Triassic to the Middle Jurassic. Neocalamites fossils are commonly found in coal-bearing sedimentary rocks of Rhaetian stage from South China and the Yanchang G...
supported by the National Science Foundation of China(grants No.41272213,41572177,41573023,41502193 and 41272222)
The Qinling Orogenic Belt(QOB)is a composite continental orogenic belt that has experienced many tectonic events.The QOB is subdivided into the following three litho-tectonic units:the North Qinling terrane,the Middle...
financially supported by the China Postdoctoral Science Foundation(grant 2017M610960);China Geological Survey(grants No.DD20160346 and DD20160055)
Objective In recent years, a series of tungsten prospecting breakthroughs have been made in the southern Qinling Mountains. Especially, a new deposit type with a scheelite -beryl-molybdenite assemblage in the Zhen'a...
financially supported by the National Natural Science Foundation of China(grants No. 41573036 and 41030423);the Xiangtanzi Gold Deposit Prospecting Program of the Zhaojin Mining Industry Company Limited(3-4-2016-061)
Objective The western Qinling belongs to the western part of the Qinling-Dabie-Sulu orogen between the North China Block and South China Block. Multiple orogenic events might be responsible for different types of gold...
supported by the National Science Foundation of China (grants No.41272213 and 41572177)
Objective The Qinling orogenic belt is a typical complex continental orogenic belt which has experienced multiperiod tectonic evolution and where some important tectonic belts formed.The Luoluan fault is one of the mo...