The Paleoproterozoic was a critical time in whether modern-style plate tectonics had become globally dominant(e.g.,Wan et al.,2020).The Capricorn Orogen witnessed the assembly of the Pilbara and Yilgarn Cratons and an...
supported by the Key Laboratory of Gold Mineralization Processes and Resource Utilization,MNR;Shandong Provincial Key Laboratory of Metallogenic Geological Process and Resource Utilization(Grant No.KFKT202103);National Natural Science Foundation of China(Grant No.41876037)。
Feldspar Pb isotopes have been widely used to trace magmatic formation and evolution processes.However,it remains unclear whether post-magmatic thermal events can affect feldspar Pb isotopic ratios.Here,the in situ Pb...
granted by the National Natural Science Foundation of China(Grant Nos.41872194,41872203);the Regional Geological Survey Project of Huai′an,Hebei-Liangcheng,Inner Mongolia(Grant No.DD20190035)。
We investigated the meta-gabbronorites in Liangcheng and used detailed petrography,geochemistry,zircon geochronological and in-situ Hf isotopic studies to clarify their formation and metamorphic ages,petrogenesis,tect...
funded by the National Key Research and Development Program of China(Grant No.2019YFA0708501)。
The carbon cycle is an important process that regulates Earth's evolution.We compare two typical periods,in the Paleoproterozoic and Neoproterozoic,in which many geological events occurred.It remains an open question ...
funded by the Basic Scientific Research Fund of the Institute of Geology, Chinese Academy of Geological Sciences (Grant No. J2103);National Key Research and Development Project of the Ministry of Science and Technology of China (Grant No. 2017YFC0601301);the National Natural Science Foundation of China (Grant No. 41972224);the China Geological Survey (Grant No. DD2019004)。
The Alxa Block is the westernmost part of the North China Craton(NCC), and is regarded as one of the basement components of the NCC. Its geological evolution is of great significance for the understanding of the NCC.H...
financially supported by the 3D Geological Mapping and Deep Geological Survey of the China Geological Survey under a pilot project entitled Deep Geological Survey of the Benxi–Linjiang Area (Project No. 1212011220247)
Paleoproterozoic granitoids are an important constituent of the Jiao-Liao-Ji Belt(JLJB). The spatial-temporal distribution and types of Paleoproterozoic granitoids are closely related to the evolution of the JLJB. In ...
financially supported by the National Science Foundation of China (grants No.41430207 and 90914001);the National Key Basic Research Program of China (grant No.2012CB416603);the Science Foundation of China University of Petroleum, Beijing (grant No.2462017YJRC032)
Objective The Hadean zircon and rock are critical to deepening our understanding of the developmental history of early Earth, making possible new avenues for the Pre-Archean Eon. However, the Hadean rock on Earth is ...
financially supported by the NSFC(grant no.41430207, 41602340);China Postdoctoral Science Foundation ( 2016M591246)
Tectonically emplaced peridotites from North Hebei Province, North China Craton, have retained an original harzburgite mineral assemblage of olivine (54%-58%) + orthopyroxene (40%-46%) +minor clinopyroxene (〈1...
financially supported by the National Natural Science Foundation of China(grants No.41173065 and 40703012);the China Geological Survey(grants No.1212011121075, 12120114020901,12120113094000 and 1212011120332);the Basic Outlay of Scientific Research Work from the Ministry of Science and Technology of the People's Republic of China(grant No.J1403)
The Miyun area of Beijing is located in the northern part of the North China Craton (NCC) and includes a variety of Archean granitoids and metamorphic rocks. Magmatic domains in zircon from a tonalite reveal Early N...
financially supported by the Ph.D Foundation of the Ministry of Education of China(grant No.20133402130008);the National Basic Research Program of China(grant No.2015CB856104);the National Natural Science Foundation of China(grant No.41273036)
The Precambrian basement rocks in the Bengbu and neighboring areas, located at the southeastern margin of the North China Craton, occur as granulite terrains and xenoliths in the Mesozoic dioritic porphyry.