DOI:
矿床地质:2014,Vol.>>Issue(1):70-86

云南者桑金矿床载金矿物标型特征研究
地质过程与矿产资源国家重点实验室, 中国地质大学地球科学与资源学院, 北京 100083;成都理工大学地球科学学院, 四川 成都 610059;地质过程与矿产资源国家重点实验室, 中国地质大学地球科学与资源学院, 北京 100083;成都理工大学地球科学学院, 四川 成都 610059;成都理工大学地球科学学院, 四川 成都 610059;成都理工大学地球科学学院, 四川 成都 610059
Typomorphic characteristics of gold-bearing minerals in Zhesang gold deposit, Yunnan Province
DAI HongZhang,CHEN CuiHua,GU XueXiang,LI BaoHua,DONG ShuYi,CHENG WenBin
(State Key Laboratory of Geological Processes and Resources, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, Sichuan, China)
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投稿时间:2013-01-06   修订日期:2014-01-14      网络发布日期:2014-10-23
中文摘要:者桑金矿床处在滇黔桂“金三角”构造带中,该矿床的形成经历了沉积成岩期、热液成矿期及表生氧化期,黄铁矿及毒砂为矿床的重要载金矿物。通过岩相学特征、标型矿物研究,发现热液成矿Ⅰ阶段中主要载金矿物为毒砂,热液成矿Ⅱ阶段为金矿化最主要阶段,主要载金矿物为黄铁矿。黄铁矿呈胶状、细粒状、破碎状;毒砂呈粗粒板柱状,维氏硬度偏低为其载金标型。晶胞参数测试表明,黄铁矿a值在5.4300~5.4325 Å;之间,成矿Ⅰ阶段至成矿Ⅱ阶段a值逐渐变大。载金毒砂明显富S、Co亏As,导致bcβ均低于理论值。各成矿阶段的黄铁矿及毒砂中主量、微量元素及硫同位素组成呈现一定变化规律,成矿物质主要来自于富含有机质的围岩。者桑金矿床为中低温热液矿床。
Abstract:The Zhesang gold deposit located in the structural belt of Yunnan-Guizhou-Guangxi gold triangle structural belt. The formation of the Zhesang gold deposit experienced three stages, i.e., sedimentary diagenesis, hydrothermal mineralization and supergenic oxidation. Pyrites and arsenopyrites are two major Au-bearing minerals. Petrographic and typomorphic observations reveal that arsennopyrites were formed in the hydrothermal mineralization Ⅰ phase (HMⅠ) whereas pyrites in the hydrothermal mineralization Ⅱ phase (HMⅡ), which was the primary gold formation phase. The gold-bearing pyrites are colloidal, fine-gained or fragmentized, while the gold-bearing arsenopyrites are in the coarse columnar form. Both of them have low reflectance. Lattice parameter measurement indicates that the a of pyrite is 5.4300~5.4325 Å, which gradually becomes larger from HM Ⅰ to HM Ⅱ, suggesting that As was concentrated in the hydrothermal mineralization stage. Gold-bearing arsenopyrites are rich in S, Co and poor in As and, as a result, b, c and β are lower than their theoretical values. Similarities of geochemical and S isotopic compositions between pyrites and arsenopyrites imply that organic wall rock contributed most of the metallogenic materials. It is thus concluded that the Zhesang gold deposit is a middle-low temperature hydrothermal deposit.
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基金项目:本文得到国家自然科学基金重点项目(编号:40930423);国家重点基础研究发展计划(973)(编号:2014CB440903);国家自然科学基金面上项目(编号:41372093);教育部高校博士点基金项目(编号:2009512212000);成都理工大学中青年骨干教师培养计划项目;高等教育质量工程项目《矿相学》优秀教材建设(编号:XJC1105)联合资助
引用文本:
代鸿章,陈翠华,顾雪祥,李保华,董树义,程文斌.2014.云南者桑金矿床载金矿物标型特征研究[J].矿床地质,33(1):70~86
DAI HongZhang,CHEN CuiHua,GU XueXiang,LI BaoHua,DONG ShuYi,CHENG WenBin.2014.Typomorphic characteristics of gold-bearing minerals in Zhesang gold deposit, Yunnan Province[J].Mineral Deposits33(1):70~86
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