Mantle plume-triggered rifting closely following Neoarchean cratonization revealed by 2.50-2.20 Ga magmatism across North China Craton
文献类型：期刊论文
| 作者 | Zhou, Yanyan1,2; Zhai, Mingguo1,2,3 |
| 刊名 | EARTH-SCIENCE REVIEWS
 |
| 出版日期 | 2022-07-01 |
| 卷号 | 230页码:31 |
| ISSN号 | 0012-8252 |
| 关键词 | North China Craton Neoarchean cratonization Paleoproterozoic magmatism Mantle-crustal interaction Tectonic transition Paleoproterozoic rifting |
| DOI | 10.1016/j.earscirev.2022.104060 |
| 英文摘要 | The Earth experienced fundamental tectonic transformation and paleoclimatic upheavals during the early Paleoproterozoic (2.50-2.20 Ga). However, the tectonic framework of this crucial period is challenging to define precisely because of the tectono-magmatic "slowdown ". Here we carry on a comprehensive compilation of published 2.50-2.20 Ga magmatism in the North China Craton (NCC), in order to provide key constraints on the Archean-Proterozoic transition. All the rocks can be divided into two stages including three subgroups: stage 1 (2.50-2.42 Ga), stage 2-1 (2.42-2.25 Ga), and stage 2-2 (2.25-2.20 Ga). Rocks of stage 1 are mainly gabbros, sanukitoid-like rocks, diorites, tonalite-trondhjemite-granodiorite (TTG), and potassic granites. The TTGs are medium to high pressure (MP-HP) series and likely derived from subducted slabs. The gabbros and sanukitoid-like rocks were from enriched mantle sources. The diorites and K-rich granites were from partial melting of different levels of crust. The rock associations are representative of the continuation of the Neoarchean cratonization and record a tectonic shift from subduction-collision to post-collision. The youngest high-K granites (ca. 2.42 Ga) may mark the real termination of the "Neoarchean " cratonization in the NCC. Rocks of stage 2-1 are mainly komatiitic rocks, gabbros, low-pressure (LP) TTGs, diorites, and A-type granites. Rocks of stage 2-2 comprise basalt-dacite-rhyolite and granitic anatectic melt. The komatiitic rocks likely derived from the asthenospheric mantle possibly related to a plume setting. The mafic rocks were sourced from an ancient and enriched subcontinental lithospheric mantle. The upwelling mantle-derived melts further induced partial melting of the cratonic lower to upper crust to form the LP TTGs, diorites, and A-type granites. The stage 2 rock associations were emplaced as typical intraplate magmatism, recording initiation and development of a plume-triggered rift setting. These observations are further supported by our new data on 2.32-2.27 Ga rocks in the southern NCC, including, but not limited to, LP-TTGs, gabbros, and A-type granites. Subsequently, rifting continually developed (2.20-2.10 Ga) and a tectonic transition ensued from passive to active continental margin (2.20-2.05/2.00 Ga, e.g., Peng et al., 2012) until subduction-collision-post-collision occurred (1.95-1.80 Ga; e. g., Zhao et al., 2002a, 2002b). From a global perspective, the early Paleoproterozoic tectono-magmatic events in the NCC tend to be synchronized to those of the world including rifting magmatism, and large igneous provinces (LIPs), etc. During the early Paleoproterozoic rifting processes, sulphur dioxide (e.g., SO2) was likely to be released into the atmosphere by magmatic events (e.g., LIPs), and continental uplift would have induced weathering, erosion, and delivery of bioessential nutrients to the ocean, all these were vital to the paleoenvironmental changes, lowering pCO(2) and introducing glacial conditions. |
| WOS关键词 | U-PB ZIRCON ; LIAO-JI BELT ; A-TYPE GRANITE ; TRANS-HUDSON OROGEN ; PALEOPROTEROZOIC METAVOLCANIC ROCKS ; ZHONGTIAO MOUNTAIN REGION ; HF ISOTOPIC COMPOSITIONS ; HIGH-GRADE METAMORPHISM ; EASTERN HEBEI PROVINCE ; META-MAFIC ROCKS |
| 资助项目 | Key Program of National Natural Science Foundation of China[41890831] ; National Natural Science Founda-tion of China[41972202] ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution[2019-2022] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| 出版者 | ELSEVIER |
| WOS记录号 | WOS:000812359800003 |
| 资助机构 | Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; Key Program of National Natural Science Foundation of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution ; Independent Research Project of the State Key Laboratory of Lithospheric Evolution |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/106095]  |
| 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 | Zhou, Yanyan; Zhai, Mingguo |
| 作者单位 | 1.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100049, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhou, Yanyan,Zhai, Mingguo. Mantle plume-triggered rifting closely following Neoarchean cratonization revealed by 2.50-2.20 Ga magmatism across North China Craton[J]. EARTH-SCIENCE REVIEWS,2022,230:31. |
| APA | Zhou, Yanyan,&Zhai, Mingguo.(2022).Mantle plume-triggered rifting closely following Neoarchean cratonization revealed by 2.50-2.20 Ga magmatism across North China Craton.EARTH-SCIENCE REVIEWS,230,31. |
| MLA | Zhou, Yanyan,et al."Mantle plume-triggered rifting closely following Neoarchean cratonization revealed by 2.50-2.20 Ga magmatism across North China Craton".EARTH-SCIENCE REVIEWS 230(2022):31. |
入库方式： OAI收割
来源：地质与地球物理研究所
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