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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
He, Ar, and S isotopic compositions and origin of giant porphyry Mo deposits in the Lesser Xing'an Range-Zhangguangcai Range metallogenic belt, northeast China

文献类型：期刊论文

作者Zeng, Qingdong1,2,3; Guo, Weikang1,2,3; He, Huaiyu2,3,4; Zhou, Lingli1,2; Cheng, Guohua1,2; Su, Fei2,4; Wang, Yongbin1,2; Wang, Ruiliang5
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2018-10-01
卷号165页码:228-240
关键词He Ar isotope Sulfur isotope Giant porphyry Mo deposit Lesser Xing'an Range-Zhangguangcai Range metallogenic belt Northeast China
ISSN号1367-9120
DOI10.1016/j.jseaes.2018.04.002
英文摘要The Lesser Xing'an Range-Zhangguangcai Range metallogenic belt, located at the eastern segment of the Centra Asian metallogenic domain, hosts two giant Mo porphyry deposits, the Early Jurassic Luming deposit and the Middle Jurassic Daheishan deposit. In this study, the He-Ar and S isotopic compositions of sulfides from differen, hydrothermal stages of the Daheishan and Luming deposits were determined. Fluid inclusions hosted in pyrite: shown that He-3/He-4 ratios of the Luming and Daheishan deposit range from 0.02 to 0.32 Ra, and 0.7 to 2.5 Ra respectively. Ar-40/Ar-36 ratios of the Luming and Daheishan deposit range from 313.3 to 535.1, and 309.9 tc 360.6, respectively. He and Ar isotopic compositions suggest that the ore-forming fluids of the turning deposi are mainly crustal-derived fluids, with near atmospheric Ar and crustal He values. Mantle-derived fluids are z minor component. In contrast, the ore-forming fluids of the Daheishan deposit are a mixture between a crust derived fluid and a mantle-derived fluid. The 834S values of the sulfide samples from the Luming deposi (4.98-7.14%o) and the Daheishan deposit (1.83-2.88960) indicate that the sulfur in the ore-forming fluids wa: primarily derived from granitic magma. The isotopic compositions across the stages within one deposit have nc variability. The similar He-Ar and S isotopic compositions of the sulfides from the different Mo-bearing by drothermal stages of these two giant Mo deposits indicate that the overprinting of the multiple stages of Mo bearing hydrothermal fluids may be a key factor in the formation of giant porphyry Mo deposits. Meanwhile, the westward subduction of the Paleo-Pacific plate might have played an important role for the formation of the giant Mo deposits in the Lesser Xing'an Range-Zhangguangcai Range metallogenic belt.
WOS关键词LUMING MOLYBDENUM DEPOSIT ; U-PB AGES ; NE CHINA ; JILIN PROVINCE ; GEOLOGICAL SIGNIFICANCE ; HEILONGJIANG PROVINCE ; OROGENIC BELT ; GOLD DEPOSITS ; ZIRCON U ; GENETIC-IMPLICATIONS
资助项目National Natural Science Foundation of China[41390443] ; National Key Research and Development Program of China[2017YFC0601306]
WOS研究方向Geology
语种英语
WOS记录号WOS:000449447300014
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/89463]  
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
通讯作者Zeng, Qingdong
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Coll Earth Sci, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China
5.China Univ Geosci Beijing, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
推荐引用方式
GB/T 7714		 Zeng, Qingdong,Guo, Weikang,He, Huaiyu,et al. He, Ar, and S isotopic compositions and origin of giant porphyry Mo deposits in the Lesser Xing'an Range-Zhangguangcai Range metallogenic belt, northeast China[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,165:228-240.
APA Zeng, Qingdong.,Guo, Weikang.,He, Huaiyu.,Zhou, Lingli.,Cheng, Guohua.,...&Wang, Ruiliang.(2018).He, Ar, and S isotopic compositions and origin of giant porphyry Mo deposits in the Lesser Xing'an Range-Zhangguangcai Range metallogenic belt, northeast China.JOURNAL OF ASIAN EARTH SCIENCES,165,228-240.
MLA Zeng, Qingdong,et al."He, Ar, and S isotopic compositions and origin of giant porphyry Mo deposits in the Lesser Xing'an Range-Zhangguangcai Range metallogenic belt, northeast China".JOURNAL OF ASIAN EARTH SCIENCES 165(2018):228-240.

入库方式： OAI收割

来源：地质与地球物理研究所

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