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现代地质 ›› 2025, Vol. 39 ›› Issue (03): 648-666.DOI: 10.19657/j.geoscience.1000-8527.2024.073

• 机器学习与矿物学应用 • 上一篇    下一篇

黑龙江二道坎银铅锌矿床黄铁矿标型特征及其S、Pb同位素研究

郑博1(), 李成禄1,*(), 于雷2, 杨文鹏1, 徐国战1, 史冬岩3, 杨元江1, 符安宗1, 赵瑞君1   

  1. 1.黑龙江省自然资源调查院, 黑龙江 哈尔滨 150036
    2.中国地质调查局哈尔滨自然资源综合调查中心,黑龙江 哈尔滨 150081
    3.黑龙江省矿业集团有限责任公司,黑龙江 哈尔滨 150040
  • 出版日期:2025-06-10 发布日期:2025-07-03
  • 通信作者: *李成禄,男,正高级工程师,1984年出生,主要从事金属矿产成因矿物与找矿矿物学研究工作。Email:lcl230881@163.com
  • 作者简介:郑 博,男,高级工程师,1987年出生,主要从事成矿规律、矿物学研究工作。Email:hljdcyzb1987@163.com
  • 基金资助:
    黑龙江省重点研发计划项目(GA21A204);东北区域创新联合发展基金项目(QCJJ2022-10);黑龙江省地质矿产局科研项目(HKY202301);黑龙江省地质矿产局科研项目(HKY202302);中国地质调查局地质调查项目(DD202300256)

Typomorphic Characteristics and Stable Isotopes of Pyrite from the Erdaokan Ag-Pb-Zn Deposit, Heilongjiang Province

ZHENG Bo1(), LI Chenglu1,*(), YU Lei2, YANG Wenpeng1, XU Guozhan1, SHI Dongyan3, YANG Yuanjiang1, FU Anzong1, ZHAO Ruijun1   

  1. 1. Heilongjiang Institute of Natural Resources Survey, Harbin, Heilongjiang 150036, China
    2. Harbin Center for Integrated Natural Resources Survey, CGS, Harbin, Heilongjiang 150081, China
    3. Heilongjiang Mining Group Co., Ltd., Harbin, Heilongjiang 150040, China
  • Published:2025-06-10 Online:2025-07-03

摘要:

为提取二道坎银铅锌矿床成因及找矿信息,对与成矿密切相关的黄铁矿进行主量、稀土微量元素及S、Pb同位素等研究。结果显示,黄铁矿的S/Fe、Au/Ag、Co/Ni、Fe/(S+As)和Co-Ni-As等成分标型特征显示该矿床属于中浅成火山热液型矿床,且所勘查的位置处于矿体中浅部;黄铁矿中轻稀土富集,具弱负Eu异常,无Ce异常,相对富集高场强元素Th、U、P、Hf和Yb,亏损大离子亲石元素Rb、K和Sr,Y/Ho值,显示成矿流体具有壳幔混合特征。Zr/Hf、Nb/Ta值显示成矿流体处于较稳定的环境中,但成矿过程中可能混入外来热液物质。硫同位素数值集中在+2.3‰~+8.6‰,表明成矿物质来源较深;206Pb/204Pb值为18.007~18.034,207Pb/204Pb值为15.501~15.522,208Pb/204Pb值为37.704~37.755,显示成矿物质为以地幔为主的壳幔混合来源。结合本区地球化学特征及区域典型矿床特征,认为二道坎银铅锌矿床为浅成低温热液型矿床,目前已剥蚀到中浅部,深部仍有一定的找矿潜力。

关键词: 黄铁矿, 标型特征, 稳定同位素, 矿床成因, 二道坎银铅锌矿床, 黑龙江多宝山地区

Abstract:

For the purposes of extracting genesis and prospecting information of the Erdaokan Ag-Pb-Zn deposit, a detailed investigation on chemical compositions,trace elements, rare earth element, as well as S-Pb isotopes of the pyrite related to mineralization.Genetic typomorphic characteristics of the pyrite, such as S/Fe, Au/Ag, Co/Ni, Fe/(S+As), Fe/(S+As), Co-Ni-As, etc., suggest that this deposit belongs to the intermediate to epithermal volcanic hydrothermal deposit, with the pyrite from the middle-superficial part of the prospecting orebody. The LREE are relatively more enrichment than The HREE. Eu negative anomalies are weak but Ce anomalies are not significant. Relative enrichment high field strength element(HFSE)such as Th,U,P,Hf and Yb. Loss large ion lithophile element(LILE) such as Rb, K and Sr.Ratios of Y/Ho reveal that the pyrite in the oreforming fluid closely related to the crust and mantle. The Zr/Hf and Nb/Ta values indicate that the ore-forming fluid is in a stable environment. However, there may be foreign hydrothermal substances mixed in the ore-forming process. Sulfur isotope values are concentrated in +2.3‰ to +8.6‰, it indicates that the source of ore-forming material is deep. Ratios of 206Pb/204Pb (18.007-18.034), 207Pb/204Pb (15.501-15.522), and 208Pb/204Pb (37.704-37.755), for the pyrites suggest that the ore-forming materials were sourced mainly from the mantle materials mixing with minor crustal materials.Based on the geochemical characteristics and typical deposit characteristics of this area, the Erdaokan Ag-Pb-Zn deposit is considered to be an epithermal hydrothermal silver deposit,which has been denuded to the middle and shallow part at present, and still has certain prospecting potential in the deep part.

Key words: pyrite, typomorphic characteristics, stable isotope, genesis of deposit, Erdaokan Ag-Pb-Zn deposit, Duobaoshan region of Heilongjiang Province

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