中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geology, mineralization and magma evolution of the Zuun Mod Mo-Cu deposit in Southwest Mongolia

文献类型:期刊论文

作者Altankhuyag, Gankhuyag4; Boldbaatar, Enkhjargal4; Tunnell, Bolorchimeg N.4; Sereenen, Jargalan4; Locmelis, Marek5; Li, Xiaofeng1,2; Imai, Akira3
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2023-11-01
卷号257页码:26
关键词Porphyry Mo-Cu deposit Zuun Mod Zircon U-Pb geochronology Re-Os geochronology Southwest Mongolia
ISSN号1367-9120
DOI10.1016/j.jseaes.2023.105857
英文摘要Zuun Mod is a porphyry-type Mo-Cu deposit located in the Edren terrane in Southwest Mongolia. The deposit has estimated resources of 218 Mt with an average Mo grade of 0.057% and Cu grade of 0.069%, and significant amounts of Re. The deposit is characterized by multiple pulses of magmatism and exsolution of magmatic ore fluids and associated alteration and mineralization. The timing of these events and the tectonic environment were unconstrained, and the deposit's origin remains controversial. Based on drill core and field examinations, four lithological units of the Bayanbulag intrusive complex are identified in the deposit area including quartz syenite, quartz monzonite, granodiorite, and granite. The majority of Mo mineralization at Zuun Mod occurs in sheeted and stockwork quartz veins that crosscut units of the Bayanbulag complex as well as disseminations within altered granitoids wherein the mineralized quartz veins occur with potassic and phyllic alteration selvages. Zircon U-Pb age dating for quartz monzonite and granodiorite defined the timing of magmatic events at 305.3 +/- 3.6 Ma and 301.8 +/- 2.7 Ma, respectively. Molybdenite Re-Os geochronology on grains from a quartz vein with potassic alteration selvage determined the age of Mo mineralization at 297 +/- 4.8 Ma. Lithogeochemical data of intrusive units suggest the granitoid rocks show calc-alkaline to high-K calc-alkaline, Itype, and metaluminous to slightly peraluminous affinities that formed in a post-collisional setting and were likely sourced from subduction-modified lithosphere. Lithogeochemical signatures and the tectonic environment classify Zuun Mod into neither Climax nor Endako-types, but as a Mo-rich porphyry Cu deposit.
WOS关键词RE-OS AGES ; PORPHYRY CU ; U-PB ; ARC MAGMAS ; VOLCANIC-ROCKS ; CRUSTAL GROWTH ; CALC-ALKALINE ; OYU TOLGOI ; TERRANE SUBDIVISION ; COPPER DEPOSITION
WOS研究方向Geology
语种英语
WOS记录号WOS:001082550100001
出版者PERGAMON-ELSEVIER SCIENCE LTD
源URL[http://ir.iggcas.ac.cn/handle/132A11/110741]  
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Boldbaatar, Enkhjargal
作者单位1.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing, Peoples R China
3.Kyushu Univ, Fac Engn, Dept Earth Resources Engn, Fukuoka, Japan
4.Mongolian Univ Sci & Technol, Dept Geol & Hydrogeol, Sch Geol & Min Engn, Ulaanbaatar, Mongolia
5.Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Rolla, MO USA
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Altankhuyag, Gankhuyag,Boldbaatar, Enkhjargal,Tunnell, Bolorchimeg N.,et al. Geology, mineralization and magma evolution of the Zuun Mod Mo-Cu deposit in Southwest Mongolia[J]. JOURNAL OF ASIAN EARTH SCIENCES,2023,257:26.
APA Altankhuyag, Gankhuyag.,Boldbaatar, Enkhjargal.,Tunnell, Bolorchimeg N..,Sereenen, Jargalan.,Locmelis, Marek.,...&Imai, Akira.(2023).Geology, mineralization and magma evolution of the Zuun Mod Mo-Cu deposit in Southwest Mongolia.JOURNAL OF ASIAN EARTH SCIENCES,257,26.
MLA Altankhuyag, Gankhuyag,et al."Geology, mineralization and magma evolution of the Zuun Mod Mo-Cu deposit in Southwest Mongolia".JOURNAL OF ASIAN EARTH SCIENCES 257(2023):26.

入库方式: OAI收割

来源:地质与地球物理研究所

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