IGGCAS OpenIR  > 岩石圈演化国家重点实验室
Continental crustal evolution and synchronous metallogeny through time in the North China Craton
Zhai, Mingguo1,2,3,4,5; Zhu, Xiyan4,5; Zhou, Yanyan2,5; Zhao, Lei2,5; Zhou, Ligang2,5
2020-06-01
Source PublicationJOURNAL OF ASIAN EARTH SCIENCES
ISSN1367-9120
Volume194Pages:15
AbstractThe generation and evolution of continent crust have long been matters of debates. There is evidence to support the view that the first formation of TTGs of continent was possibly before 4.4 Ga, followed by the sizable continent crust associated with BIF-bearing supra-crustal rocks at ca. 3.8 Ga. Multiple stages of continental growth include continental nuclei at similar to 3.1 Ga, enormous crustal growth at 2.9-2.7 Ga and stabilization and cratonization at similar to 2.5 Ga. Subsequently a stable super-continent was formed and the Earth was evolved into the Proterozoic eon. In the Proterozoic eon, major geological events include the great oxygen event (GOE), global rift and mobile belt event, and the Earth's middle age event with a 1.0 billion years long period of Earth's adjustment or silence. After that, the Rodinian super-continental break up event (the Nanhua rift) and subsequent Gondwana amalgamation have been suggested to be involved with mantle-plume and the modern stylelike plate tectonics, both of which are still under debates. Recent studies suggest that the continental metallogeny has secular changes with the evolving Earth, showing synchronous evolution with the continental crust through time. The North China Craton (NCC) is one of the oldest cratons in the world, and has undergone six major tectono-metallogenic cycles: (1) the Neoarchean crustal growth and Algoman-type BIFs-greenstone belt and gold metallogenic system, (2) Paleoproterozoic GOE associated with global (Huronian) rifting- Glaciation and Superior-type BIFs-Mg-B metallogenic system, (3) Paleoproterozoic rifting-subduction-accretion-collision event (mobile belt) and Cu-Pb-Zn metallogenic system; (4) Late Paleoproterozoic - Neoproterozoic multi-stage rifting and REE-Fe-Pb-Zn metallogenic system; (5) Paleozoic orogenesis at the margins of the craton and porphyry Cu-Mo metallogenic system; and (6) Mesozoic extensional tectonics associated with lithosphere thinning and intracontinental Au metallogenic systems. Ore deposit types in each of these metallogenic systems show distinct characteristics and tectonic affinities. Changes of metallogenic styles with time, from the dominant BIFs in Archean to polymetallic deposits in Proterozoic and Phanerozoic, demonstrate that the nature and style of metallogeny through time change with different stages of the Earth's evolution and are the expression of variable materials at the different stages. The changes of metallogeny through time are controlled by the irreversible continental tectonic evolution. The connotation and signification of synchronous evolution of continental crust and mineral deposit systems through time are beyond the study of mineral resources but would provide new insights into the geodynamics of the generation and evolution of the continent. The NCC provides an excellent venue to address the linkage between metallogenic processes and secular changes in the Earth System, including mantle dynamics and crust-mantle interaction on a global perspective.
KeywordSynchronous evolution Continental crust Metallogeny North China Craton (NCC)
DOI10.1016/j.jseaes.2019.104169
Funding OrganizationNational Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea
WOS KeywordZIRCON U-PB ; JIAODONG GOLD PROVINCE ; BANDED IRON FORMATIONS ; GREAT OXIDATION EVENT ; ORE-FORMING FLUIDS ; LIAO-JI BELT ; INNER-MONGOLIA ; PLATE-TECTONICS ; GEOCHRONOLOGICAL CONSTRAINTS ; THERMAL REGIMES
Language英语
Funding ProjectNational Nature Science Foundation of China[41890834] ; National Nature Science Foundation of China[41530208] ; Chinese Academy of Sciences[QYZDY-SSW-DQC017] ; Chinese Academy of Sciences[XDB 18030205] ; National Research Foundation of Korea[NRF-2017R1A2B2011224] ; National Research Foundation of Korea[NRF-2017K1A1A201380]
Funding OrganizationNational Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea ; National Research Foundation of Korea
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000538820400007
PublisherPERGAMON-ELSEVIER SCIENCE LTD
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/96911
Collection岩石圈演化国家重点实验室
矿产资源研究院重点实验室
Corresponding AuthorZhai, Mingguo
Affiliation1.Northwest Univ, State Key Lab Continental Geodynam, Xian 710069, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithosphere Evolut, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth Sci, Key Lab Computat Earth Dynam, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
5.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100049, Peoples R China
First Author AffilicationInstitute of Geology and Geophysics, Chinese Academy of Sciences;  Key Laboratory of Mineral Resources, Chinese Academy of Sciences
Corresponding Author AffilicationInstitute of Geology and Geophysics, Chinese Academy of Sciences;  Key Laboratory of Mineral Resources, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Zhai, Mingguo,Zhu, Xiyan,Zhou, Yanyan,et al. Continental crustal evolution and synchronous metallogeny through time in the North China Craton[J]. JOURNAL OF ASIAN EARTH SCIENCES,2020,194:15.
APA Zhai, Mingguo,Zhu, Xiyan,Zhou, Yanyan,Zhao, Lei,&Zhou, Ligang.(2020).Continental crustal evolution and synchronous metallogeny through time in the North China Craton.JOURNAL OF ASIAN EARTH SCIENCES,194,15.
MLA Zhai, Mingguo,et al."Continental crustal evolution and synchronous metallogeny through time in the North China Craton".JOURNAL OF ASIAN EARTH SCIENCES 194(2020):15.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[Zhai, Mingguo]'s Articles
[Zhu, Xiyan]'s Articles
[Zhou, Yanyan]'s Articles
Baidu academic
Similar articles in Baidu academic
[Zhai, Mingguo]'s Articles
[Zhu, Xiyan]'s Articles
[Zhou, Yanyan]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Zhai, Mingguo]'s Articles
[Zhu, Xiyan]'s Articles
[Zhou, Yanyan]'s Articles
Terms of Use
No data!
Social Bookmark/Share
Add to CiteULike Add to Connotea Add to Del.icio.us Add to Digg Add to Reddit Add to Technorati
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.