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热液型金矿床中的黄铁矿矿物学研究综述

高永伟, 王志华, 黎卫亮, 张振亮

高永伟, 王志华, 黎卫亮, 等. 热液型金矿床中的黄铁矿矿物学研究综述[J]. 西北地质, 2019, 52(3): 58-69. DOI: 10.19751/j.cnki.61-1149/p.2019.03.006
引用本文: 高永伟, 王志华, 黎卫亮, 等. 热液型金矿床中的黄铁矿矿物学研究综述[J]. 西北地质, 2019, 52(3): 58-69. DOI: 10.19751/j.cnki.61-1149/p.2019.03.006
shu
GAO Yongwei, WANG Zhihua, LI Weiliang, et al. A Review of Pyrite Mineralogy Research in Hydrothermal Gold Deposits[J]. Northwestern Geology, 2019, 52(3): 58-69. DOI: 10.19751/j.cnki.61-1149/p.2019.03.006
Citation: GAO Yongwei, WANG Zhihua, LI Weiliang, et al. A Review of Pyrite Mineralogy Research in Hydrothermal Gold Deposits[J]. Northwestern Geology, 2019, 52(3): 58-69. DOI: 10.19751/j.cnki.61-1149/p.2019.03.006
shu

热液型金矿床中的黄铁矿矿物学研究综述

  • 中国地质调查局西安地质调查中心/西北地质科技创新中心, 自然资源部岩浆作用成矿与找矿重点实验室, 陕西 西安 710054

基金项目: 

国家自然科学基金项目“西天山卡特巴阿苏金矿床黄铁矿特征研究及其对成矿机制的指示”（41602096）、“西天山智博火山岩型铁矿床矿化蚀变机制研究”（41402079），中国地质调查局项目“商丹—大柴旦地区区域地质调查”（DD20190069）

详细信息
    作者简介:

    高永伟(1986-),男,硕士,高级工程师,矿床学专业,主要从事西北地区区域地质矿产调查及综合研究工作。E-mail:gaoyw21033@126.com

  • 中图分类号: P578.2

A Review of Pyrite Mineralogy Research in Hydrothermal Gold Deposits

  • Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, Xi'an Center of China Geological Survey/Northwest China Center for Geoscience Innovation, Xi'an 710054, Shaanxi, China

摘要

    摘要
  • 摘要: 黄铁矿是热液金矿化体系中较为重要的矿物。黄铁矿精细矿物学研究是热液金矿床成矿机制研究的一个重要课题。黄铁矿的矿物学特征主要包括物理结构和化学成分特征。笔者综述了黄铁矿的形态、晶胞参数及热电性等物理结构特征和地球化学成分特征在热液金矿床的应用及其研究进展。黄铁矿的物理特征及其时空变化规律，可以定性约束成矿物理化学条件的演化过程。黄铁矿的微量和稀土元素组成、分布及演化特征，可以示踪成矿物质及成矿流体来源，进而获得有关矿床成因及金属沉淀机制等方面的信息。此外，近年来发展迅速的黄铁矿单矿物Re-Os同位素定年及原位微区稳定同位素（S、Pb）分析可以对确定金矿床精确成矿年代及精细成矿过程提供重要的参考信息。
    Abstract: Pyrite is one of the most important minerals in hydrothermal gold mineralization systems. The research on detailed mineralogy of pyrite has become a key topic in the study of metallogenic mechanism. The mineralogical characteristics of pyrite mainly include physical structure and chemical composition features. In this paper, the application and progress on the physical characteristics (such as crystal morphology, cell parameters, thermoelectricity) and geochemical characteristics of pyrite in hydrothermal gold deposits have been reviewed. The physical features of pyrite and its time-space variation law can be used to constrain qualitatively the evolution process of mineralization physicochemical conditions. The composition, distribution and evolution characteristics of REE and trace elements are effective tools for tracing the source of ore-forming materials and fluids, and then obtaining information on the genesis of the deposit and the mechanism of metal precipitation. Moreover, with the rapid innovation of analysis techniques, pyrite Re-Os isotopic dating and in situ S-Pb isotope analyses also provide important reference information on determining the precise metallogenic age and specific ore-forming process of hydrothermal gold deposits.
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