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  2. 地质与地球物理研究所
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  4. 中国科学院矿产资源研究重点实验室
Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing'an Range W belt, NE China: insights from the Narenwula Complex

文献类型：期刊论文

作者Xie, Wei1,4,5; Zeng, Qing-Dong1,4,5; Yang, Jin-Hui1,5,6; Li, Rui1,5,6; Zhang, Zhuang2; Wang, Rui-Liang3; Wu, Jin-Jian1,4,5
刊名GEOLOGICAL MAGAZINE
出版日期2022-01-10
页码35
关键词zircon U-Pb ages Hf isotopes geochemistry Narenwula complex Great Xing'an Range NE China
ISSN号0016-7568
DOI10.1017/S0016756821001175
英文摘要Extensive magmatism in NE China, eastern Central Asian Orogenic Belt, has produced multi-stage granitic plutons and accompanying W mineralization. The Narenwula complex in the southwestern Great Xing'an Range provides important insights into the petrogenesis, geodynamic processes and relationship with W mineralization. The complex comprises granodiorites, monzogranites and granite porphyry. Mafic microgranular enclaves are common in the granodiorites, and have similar zircon U-Pb ages as their host rocks (258.5-253.9 Ma), whereas the W-bearing granitoids yield emplacement ages of 149.8-148.1 Ma. Permian granodiorites are I-type granites that are enriched in large-ion lithophile elements and light rare earth elements, and depleted in high field strength elements and heavy rare earth elements. Both the mafic microgranular enclaves and granodiorites have nearly identical zircon Hf isotopic compositions. The results suggest that the mafic microgranular enclaves and granodiorites formed by the mixing of mafic and felsic magmas. W-bearing granitoids are highly fractionated A-type granites, enriched in Rb, Th, U and Pb, and depleted in Ba, Sr, P, Ti and Eu. They have higher W concentrations and Rb/Sr ratios, and lower Nb/Ta, Zr/Hf and K/Rb ratios than the W-barren granodiorites. These data and negative epsilon(Hf)(t) values (-6.0 to -2.1) suggest that they were derived from the partial melting of ancient lower crust and subsequently underwent extreme fractional crystallization. Based on the regional geology, we propose that the granodiorites were generated in a volcanic arc setting related to the subduction of the Palaeo-Asian Ocean, whereas the W-bearing granitoids and associated deposits formed in a post-orogenic extensional setting controlled by the Mongol-Okhotsk Ocean and Palaeo-Pacific Ocean tectonic regimes.
WOS关键词ZIRCON U-PB ; S-TYPE GRANITES ; A-TYPE GRANITES ; MONGOL-OKHOTSK OCEAN ; SOLONKER SUTURE ZONE ; ASIAN OROGENIC BELT ; LACHLAN FOLD BELT ; WURINITU MOLYBDENUM DEPOSIT ; TIN-POLYMETALLIC DEPOSIT ; CENTRAL INNER-MONGOLIA
资助项目National Natural Science Foundation of China[91962104]
WOS研究方向Geology
语种英语
WOS记录号WOS:000740924800001
出版者CAMBRIDGE UNIV PRESS
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 ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/103975]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
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Zeng, Qing-Dong
作者单位1.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
2.Chifeng Chaihulanzi Gold Min Co Ltd, Chifeng 024000, Peoples R China
3.China Univ Geosci Beijing, Fac Geosci & Resources, Beijing 100083, 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 100029, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Xie, Wei,Zeng, Qing-Dong,Yang, Jin-Hui,et al. Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing'an Range W belt, NE China: insights from the Narenwula Complex[J]. GEOLOGICAL MAGAZINE,2022:35.
APA Xie, Wei.,Zeng, Qing-Dong.,Yang, Jin-Hui.,Li, Rui.,Zhang, Zhuang.,...&Wu, Jin-Jian.(2022).Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing'an Range W belt, NE China: insights from the Narenwula Complex.GEOLOGICAL MAGAZINE,35.
MLA Xie, Wei,et al."Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing'an Range W belt, NE China: insights from the Narenwula Complex".GEOLOGICAL MAGAZINE (2022):35.

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来源：地质与地球物理研究所

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