中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geochemistry and chronology of the early Paleozoic diorites and granites in the Huangtupo volcanogenic massive sulfide (VMS) deposit, Eastern Tianshan, NW China: Implications for petrogenesis and geodynamic setting

文献类型:期刊论文

作者Zheng, Jiahao1,2; Chai, Fengmei3; Feng, Wanyi2; Yang, Fuquan4; Shen, Ping1
刊名LITHOS
出版日期2018-03-01
卷号302页码:455-466
关键词Huangtupo Vms Deposit Granites And Diorites Eastern Tianshan Early Paleozoic Geodynamic Setting
ISSN号0024-4937
DOI10.1016/j.lithos.2018.01.022
文献子类Article
英文摘要The Eastern Tianshan orogen contains many late Paleozoic porphyry Cu and magmatic Cu-Ni deposits. Recent studies demonstrate that several early Paleozoic volcanogenic massive sulfide (VMS) Cu-polymetallic and porphyry Cu deposits were discovered in the northern part of Eastern Tianshan. This study presents zircon U-Pb, whole-rock geo-chemical, and Sr-Nd isotopic data for granites and diorites from the Huangtupo VMS Cu-Zn deposit, northern part of the Eastern Tianshan. Our results can provide constraints on the genesis of intermediate and felsic intrusions as well as early Paleozoic geodynamic setting of the northern part of Eastern Tianshan. LA-ICP-MS zircon U-Pb analyses suggest that the granites and diorites were formed at 435 +/- 2 Ma and 440 +/- 2 Ma, respectively. Geochemical characteristics suggest that the Huangtupo granites and diorites are metaluminous rocks, exhibiting typical subduction-related features such as enrichment in LILE and LREE and depletion in HFSE. The diorites have moderate Mg#, positive epsilon(Nd)(t) values (+6.4 to +73), and young Nd model ages, indicative of a depleted mantle origin. The granites exhibit mineral assemblages and geochemical characteristics of I-type granites, and they have positive epsilon(Nd)(t) values (+6.7 to +10.2) and young Nd model ages, suggesting a juvenile crust origin. The early Paleozoic VMS Cu-polymetallic and porphyry Cu deposits in the northern part of Eastern Tianshan were genetically related. The formation of the early Paleozoic magmatic rocks as well as VMS and porphyry Cu deposits in the northern part of Eastern Tianshan was due to a southward subduction of the Junggar oceanic plate. (C) 2018 Elsevier B.V. All rights reserved.
WOS关键词ZIRCON U-PB ; MAFIC-ULTRAMAFIC INTRUSIONS ; ASIAN OROGENIC BELT ; NATURAL REFERENCE MATERIAL ; A-TYPE GRANITOIDS ; NORTHWEST CHINA ; IRON DEPOSIT ; GEOLOGICAL SIGNIFICANCE ; CONTINENTAL GROWTH ; MO DEPOSIT
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
WOS记录号WOS:000428497500029
出版者ELSEVIER SCIENCE BV
资助机构NSFC(U1403391) ; NSFC(U1403391) ; National Key R&D Program of China(2017YFC0601201) ; National Key R&D Program of China(2017YFC0601201) ; Ministry of Land and Resources Public Welfare Industry Special Funds for Scientific Research Project(201211073) ; Ministry of Land and Resources Public Welfare Industry Special Funds for Scientific Research Project(201211073) ; China Postdoctoral Science Foundation(2016LH0003 ; China Postdoctoral Science Foundation(2016LH0003 ; 2017M610984) ; 2017M610984) ; NSFC(U1403391) ; NSFC(U1403391) ; National Key R&D Program of China(2017YFC0601201) ; National Key R&D Program of China(2017YFC0601201) ; Ministry of Land and Resources Public Welfare Industry Special Funds for Scientific Research Project(201211073) ; Ministry of Land and Resources Public Welfare Industry Special Funds for Scientific Research Project(201211073) ; China Postdoctoral Science Foundation(2016LH0003 ; China Postdoctoral Science Foundation(2016LH0003 ; 2017M610984) ; 2017M610984) ; NSFC(U1403391) ; NSFC(U1403391) ; National Key R&D Program of China(2017YFC0601201) ; National Key R&D Program of China(2017YFC0601201) ; Ministry of Land and Resources Public Welfare Industry Special Funds for Scientific Research Project(201211073) ; Ministry of Land and Resources Public Welfare Industry Special Funds for Scientific Research Project(201211073) ; China Postdoctoral Science Foundation(2016LH0003 ; China Postdoctoral Science Foundation(2016LH0003 ; 2017M610984) ; 2017M610984) ; NSFC(U1403391) ; NSFC(U1403391) ; National Key R&D Program of China(2017YFC0601201) ; National Key R&D Program of China(2017YFC0601201) ; Ministry of Land and Resources Public Welfare Industry Special Funds for Scientific Research Project(201211073) ; Ministry of Land and Resources Public Welfare Industry Special Funds for Scientific Research Project(201211073) ; China Postdoctoral Science Foundation(2016LH0003 ; China Postdoctoral Science Foundation(2016LH0003 ; 2017M610984) ; 2017M610984)
源URL[http://ir.iggcas.ac.cn/handle/132A11/88349]  
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Zheng, Jiahao; Chai, Fengmei
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China
3.Xinjiang Univ, Coll Geol & Min Engn, Xinjiang Key Lab Geodynam Proc & Metallogen Progn, Urumqi 830046, Peoples R China
4.CAGS, Inst Mineral Resources, MLR Key Lab Metallogeny & Mineral Assessment, Beijing 100037, Peoples R China
推荐引用方式
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Zheng, Jiahao,Chai, Fengmei,Feng, Wanyi,et al. Geochemistry and chronology of the early Paleozoic diorites and granites in the Huangtupo volcanogenic massive sulfide (VMS) deposit, Eastern Tianshan, NW China: Implications for petrogenesis and geodynamic setting[J]. LITHOS,2018,302:455-466.
APA Zheng, Jiahao,Chai, Fengmei,Feng, Wanyi,Yang, Fuquan,&Shen, Ping.(2018).Geochemistry and chronology of the early Paleozoic diorites and granites in the Huangtupo volcanogenic massive sulfide (VMS) deposit, Eastern Tianshan, NW China: Implications for petrogenesis and geodynamic setting.LITHOS,302,455-466.
MLA Zheng, Jiahao,et al."Geochemistry and chronology of the early Paleozoic diorites and granites in the Huangtupo volcanogenic massive sulfide (VMS) deposit, Eastern Tianshan, NW China: Implications for petrogenesis and geodynamic setting".LITHOS 302(2018):455-466.

入库方式: OAI收割

来源:地质与地球物理研究所

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