Late Neoarchean to early Paleoproterozoic tectonic evolution of the southern North China Craton: Evidence from geochemistry, zircon geochronology and Hf isotopes of felsic gneisses from the Taihua complex
文献类型：期刊论文
| 作者 | Jia, Xiao-Liang1,2; Zhai, Ming-Guo3,4; Xiao, Wen-jiao1,2,3; Sun, Yong4; Ratheesh-Kumar, R. T.1,2; Yang, He1,2; Zhou, Ke-Fa1,2; Wu, Jia-Lin5 |
| 刊名 | PRECAMBRIAN RESEARCH
 |
| 出版日期 | 2019-06-15 |
| 卷号 | 326页码:222-239 |
| 关键词 | Felsic gneisses Zircon U-Pb-Hf isotopic composition Crustal evolution Taihua complex North China Craton |
| ISSN号 | 0301-9268 |
| DOI | 10.1016/j.precamres.2017.11.013 |
| 英文摘要 | The Archean-Paleoproterozoic Taihua Complex, extending from east to west along the southern margin of the North China Craton (NCC), is an ideal window to understand the tectonic evolution of the early Earth. Here we present new data on petrology, zircon geochronology, whole-rock geochemistry and isotopes of TTGs, granitic gneisses and felsic leucosomes of migmatites from the Taihua complex in the Xiaoqinling area. Zircon LA-ICP-MS analyses of rocks yield the formation ages of 2564-2503 Ma for TTGs, 2481-2476 Ma for felsic leucosomes and 2359-2334 Ma for granitic gneisses, respectively. The zircon Lu-Hf isotopes suggest that crustal growth occurred in the late Neoarchean and crustal reworking occurred in the end of Neoarchean and the early Paleoproterozoic. The TTG gneisses are characterized by high Na2O/K2O, La/Yb, Sr/Y and low Nb/Ta ratios, and they were likely generated by partial melting of subducted juvenile oceanic crust with garnet or amphibole in residuals, a mechanism similar to the slab melting model. Both the felsic leucosomes and granitic gneisses have high SiO2 contents and various Hf isotopic compositions, and they probably were formed in an extensional setting, attributing to partial melting as well as mixing of the preexisting TTG suite. Statistically, we report a major transitional phase in the tectonic milieu of the southern NCC from compression to extension during the late Neoarchean (ca. 2.57-2.42 Ga). The compressional tectonics can be attributed to amalgamation of micro-continental blocks during the late Neoarchean (ca. 2.57-2.5 Ga) as the leading period of crustal growth and associated multistage TTG magmatism. In contrast, the extensional phase occurred during the end of Neoarchean (ca. 2.5-2.42 Ga) that may represent the end of cratonic stabilization period and formation of large amounts of K-rich granitic rocks, widespread high-grade metamorphism and migmatites. Additionally, the formation of a large amount of crust-derived granites and mafic dykes during the early Paleoproterozoic in southern NCC reflect another stage (ca. 2.36-2.24 Ga) of crustal extension, which represents an episode of initial worldwide rifting events probably linking to the great oxygen event (GOE). Therefore, the present study proposes a new profile on multi-stage crustal growth/reworking and craton stabilization during Neoarchean-Paleoproterozoic period along the southern NCC, and provides useful insights on complex and heterogeneous evolutionary processes of early Earth. |
| WOS关键词 | A-TYPE GRANITES ; U-PB AGES ; TRONDHJEMITE-GRANODIORITE TTG ; EARLY CONTINENTAL-CRUST ; LACHLAN FOLD BELT ; LU-HF ; SOUTHEASTERN MARGIN ; METAMORPHIC ROCKS ; XIAOQINLING AREA ; EXPERIMENTAL CONSTRAINTS |
| 资助项目 | National Basic Research Program of China (China 973 Program)[2012CB416606] ; Chinese Academy of Sciences (CAS) "Light of West China" Program[Y637101001] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000469157300013 |
| 出版者 | ELSEVIER SCIENCE BV |
| 资助机构 | National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; National Basic Research Program of China (China 973 Program) ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program ; Chinese Academy of Sciences (CAS) "Light of West China" Program |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/92250]  |
| 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 | Zhai, Ming-Guo |
| 作者单位 | 1.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Xinjiang Res Ctr Mineral Resources, Urumqi 830011, Xinjiang, Peoples R China 2.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi 830011, Xinjiang, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 4.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Shaanxi, Peoples R China 5.Changan Univ, Sch Earth Sci & Resources, Xian 710054, Shaanxi, Peoples R China |
| 推荐引用方式 GB/T 7714 | Jia, Xiao-Liang,Zhai, Ming-Guo,Xiao, Wen-jiao,et al. Late Neoarchean to early Paleoproterozoic tectonic evolution of the southern North China Craton: Evidence from geochemistry, zircon geochronology and Hf isotopes of felsic gneisses from the Taihua complex[J]. PRECAMBRIAN RESEARCH,2019,326:222-239. |
| APA | Jia, Xiao-Liang.,Zhai, Ming-Guo.,Xiao, Wen-jiao.,Sun, Yong.,Ratheesh-Kumar, R. T..,...&Wu, Jia-Lin.(2019).Late Neoarchean to early Paleoproterozoic tectonic evolution of the southern North China Craton: Evidence from geochemistry, zircon geochronology and Hf isotopes of felsic gneisses from the Taihua complex.PRECAMBRIAN RESEARCH,326,222-239. |
| MLA | Jia, Xiao-Liang,et al."Late Neoarchean to early Paleoproterozoic tectonic evolution of the southern North China Craton: Evidence from geochemistry, zircon geochronology and Hf isotopes of felsic gneisses from the Taihua complex".PRECAMBRIAN RESEARCH 326(2019):222-239. |
入库方式： OAI收割
来源：地质与地球物理研究所
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