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  2. 地质与地球物理研究所
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  4. 岩石圈演化国家重点实验室
Geological evolution of the North China Craton in the first billion years of Earth's history

文献类型：期刊论文

作者Liou, Peng1; Guo, Jinghui1,2; Peng, Peng1,2; Zhai, Mingguo1,2
刊名EARTH-SCIENCE REVIEWS
出版日期2023-12-01
卷号247页码:16
关键词North China Craton NCC Hadean Eoarchean Archean Crustal evolution
ISSN号0012-8252
DOI10.1016/j.earscirev.2023.104608
英文摘要During the first billion years of Earth's history (4.6-3.6 Ga), geological events such as accretion, differentiation, and impacts played a crucial role in directing Earth towards a habitable planet. Crustal rocks formed in the first billion years cover only a few parts per million of the current Earth's surface area but could provide a glimpse into early Earth processes. To date, ten sites have been identified on the Chinese mainland that contain Hadean zircons (>= 4 Ga), and five sites have been found where Eoarchean rocks (>= 3.6 Ga) are exposed. The North China Craton (NCC) preserves the possibly oldest sedimentary rocks of China (i.e., Caozhuang fuchsite-bearing quartzites in the Eastern Hebei), most of the oldest detrital/xenocrystic zircons and most of the oldest magmatic rocks of China, e.g., the ca. 3.8 Ga trondhjemites in Anshan region, the ca. 3.78 Ga granodiorites in the Eastern Hebei area, and the 3.82 Ga felsic granulite xenoliths in the Xinyang region, Henan province. These ancient minerals and rocks provide insight into the early evolutionary processes of the NCC. The positive mu 182W and mu 142Nd anomalies in the Eoarchean Anshan trondhjemites as well as the widespread Hadean detrital/xenocryst zircons provide evidence for the Hadean crust-mantle-core differentiation events that were record in the NCC. The Cr-rich fuchsite quartzites in the Caozhuang supracrustal sequence, the possibly oldest sedimentary rock in China, preserve a large quantity of the Eoarchean zircons and may document the joint contribution of juvenile ultramafic-mafic and felsic crust addition in the early earth. Most of the epsilon Hf(t) values of the Eoarchean zircons spread along the chondritic evolutionary line. Given the possibility of potential systematic biases in zircon petrogenesis and the much longer residence time for the early mafic crust, the non-depleted zircon Hf isotopes do not contradict the depleted mu 142Nd values and may imply the existence of depleted mantle and continental crust at that time. Based on the zircon Hf-O isotopes and the wide distribution of the Hadean-Eoarchean zircons, it appears that nearly all the Archean granitoid rocks from the NCC are enveloped by the evolutionary line of the depleted mantle and the mafic rocks started from 3.9 to 4.0 Ga. The Hf isotope signatures and the widespread HadeanEoarchean zircons in the NCC may indicate that the Hadean-Eoarchean (4.1-3.8 Ga) crust has been involved into formation of the Archean continent of the NCC.
WOS关键词ANSHAN-BENXI AREA ; SHRIMP U-PB ; NUVVUAGITTUQ SUPRACRUSTAL BELT ; ARCHEAN CRUSTAL EVOLUTION ; HF ISOTOPE SYSTEMATICS ; EASTERN HEBEI PROVINCE ; EARLY SILICATE EARTH ; ZIRCON LU-HF ; DETRITAL ZIRCONS ; TERRESTRIAL CRUST
资助项目National Natural Science Foundation of China[42220104008] ; National Natural Science Foundation of China[42272226] ; National Natural Science Foundation of China[92162323] ; National Natural Science Foundation of China[41890834] ; IGGCAS[IGGCAS-202204] ; IGGCAS[SKL-Z202202]
WOS研究方向Geology
语种英语
WOS记录号WOS:001112507100001
出版者ELSEVIER
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; IGGCAS ; IGGCAS ; IGGCAS ; IGGCAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; IGGCAS ; IGGCAS ; IGGCAS ; IGGCAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; IGGCAS ; IGGCAS ; IGGCAS ; IGGCAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; IGGCAS ; IGGCAS ; IGGCAS ; IGGCAS
源URL[http://ir.iggcas.ac.cn/handle/132A11/111156]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Liou, Peng
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714		 Liou, Peng,Guo, Jinghui,Peng, Peng,et al. Geological evolution of the North China Craton in the first billion years of Earth's history[J]. EARTH-SCIENCE REVIEWS,2023,247:16.
APA Liou, Peng,Guo, Jinghui,Peng, Peng,&Zhai, Mingguo.(2023).Geological evolution of the North China Craton in the first billion years of Earth's history.EARTH-SCIENCE REVIEWS,247,16.
MLA Liou, Peng,et al."Geological evolution of the North China Craton in the first billion years of Earth's history".EARTH-SCIENCE REVIEWS 247(2023):16.

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来源：地质与地球物理研究所

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