| 冈底斯成矿带西段鲁尔玛斑岩型铜（金）矿床的成矿物质来源研究 |
| Received:October 08, 2018 Revised:April 22, 2019 点此下载全文 |
| 引用本文：LIU Hong,LI GuangMing,HUANG HanXiao,ZHANG LinKui,LÜ MengHong,LAN ShuangShuang,FU JianGang,ZHOU WeiDe,XIE Hui.2019.Sources of ore-forming materials of Luerma porphyry copper (gold) deposit, western Gangdise[J].Mineral Deposits,38(3):631~643 |
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| Author Name | Affiliation | E-mail | | LIU Hong | Chengdu Center, China Geological Survey, Chengdu 610082, Sichuan, China | | | LI GuangMing | Chengdu Center, China Geological Survey, Chengdu 610082, Sichuan, China | | | HUANG HanXiao | Chengdu Center, China Geological Survey, Chengdu 610082, Sichuan, China | hanxiaohuang@126.com | | ZHANG LinKui | Chengdu Center, China Geological Survey, Chengdu 610082, Sichuan, China | | | LÜ MengHong | Sichuan Institute of Metallurgical Geology & Exploration, Chengdu 610051, Sichuan, China | | | LAN ShuangShuang | Sichuan Institute of Metallurgical Geology & Exploration, Chengdu 610051, Sichuan, China | | | FU JianGang | Chengdu Center, China Geological Survey, Chengdu 610082, Sichuan, China | | | ZHOU WeiDe | Sichuan Institute of Metallurgical Geology & Exploration, Chengdu 610051, Sichuan, China | | | XIE Hui | Sichuan Institute of Metallurgical Geology & Exploration, Chengdu 610051, Sichuan, China | |
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| 基金项目:本文为国家重点研发计划（编号：SQ2018YFC060162c、2016YFC0600308）、中国地质调查项目（编号：DD20160015、DD20190542、DD20190147）、中国科学院战略性先导科技专项（编号：XDA20070304）和西南地质科技创新中心青藏高原国际大学科计划联合资助的成果 |
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| 中文摘要:西藏措勤县鲁尔玛铜（金）矿床为冈底斯成矿带西段新发现的斑岩型矿床，位于中拉萨微陆块的西部，矿体主要呈脉状和不规则状产于含矿斑岩顶部和接触带，矿床形成于晚三叠世（213 Ma）。文章通过研究主成矿阶段硫化物的S-Pb同位素组成特征，并与晚三叠世含矿斑岩体Pb同位素组成进行对比，发现共生硫化物δ34SV-CDT值变化范围较窄（δ34SV-CDT=-2.38‰~1.75‰，极差为4.13‰，均值为-0.64‰），具有深源硫（地幔或下地壳）的特征；共生硫化物（黄铁矿、黄铜矿和毒砂等） Pb同位素（n（206Pb）/n（204Pb）、n（207Pb）/n（204Pb）、n（208Pb）/n（204Pb）分别为18.450~18.903、15.602~15.669、38.637~39.424）和晚三叠世含矿斑岩的Pb同位素（n（206Pb）/n（204Pb）、n（207Pb）/n（204Pb）、n（208Pb）/n（204Pb）分别为18.845~19.560、15.634~15.689、39.273~40.211）具有一致的线性演化曲线，显示出壳幔混合的特征，暗示鲁尔玛铜（金）矿的铅来自于晚三叠世的岩浆活动。研究认为，鲁尔玛铜（金）矿床形成于晚三叠世新特提斯洋壳向北俯冲的环境，成矿物质应源于新生地壳熔融形成的中酸性岩浆。 |
| 中文关键词:地球化学 物质来源 原位微区稳定同位素 鲁尔玛 斑岩型矿床 冈底斯 |
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| Sources of ore-forming materials of Luerma porphyry copper (gold) deposit, western Gangdise |
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| Abstract:The Late Triassic Luerma copper (gold) deposit formed at ca. 213 Ma is located in Coqen County of southern Lhasa microterrane. The orebodies are hosted in the Late Triassic intermediate-acid intrusive rocks. In this study, the authors investigated the S and Pb isotopes from pyrite, chalcopyrite, arsenopyrite and ore-bearing porphyry to understand the genesis of the Luerma deposit. The δ34Sv-CDT values in sulfide minerals range from -2.38‰ to 1.75‰ with a mean value of -0.64‰, which displays a deep sulfur source. Sulfide minerals in the Luerma deposit yielded the Pb isotope values of n(206Pb)/n(204Pb) ranging from 18.450 to 19.903, n(207Pb)/n(204Pb) ranging from 15.602 to 15.669, and n(208Pb)/n(204Pb) ranging from 38.637 to 39.424, consistent with values of of porphyry whose n(206Pb)/n(204Pb) ratios range from 18.845 to 18.560, n(207Pb)/n(204Pb) ratios range from 15.634 to 15.689, and n(208Pb)/n(204Pb) ratios range from 39.273 to 40.211. These Pb isotopes form a linear evolution curve, suggesting that fluids might have been derived from the Late Triassic magmatism. It is thus held that the oreforming materials in the Luerma deposit were mainly derived from the Late Triassic magmatism, which was likely related to the northward subduction of Paleo-Tethys oceanic crust. |
| keywords:geochemistry source of ore-forming materials in-situ microanalysis stable isotopes Luerma porphyry deposit Gangdise |
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