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现代矿业 ›› 2020, Vol. 36 ›› Issue (06): 30-.

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大红山铜矿床伴生金银矿化富集规律及找矿方向研究

金鑫1余璨2   

  1. 1.玉溪矿业有限公司;2.中国有色金属工业昆明勘察设计研究院有限公司
  • 出版日期:2020-06-25 发布日期:2021-09-14

Mineralization Enrichment Regularity and Ore Prospecting of Associated Goldsilver for Dahongshan Ironcopper Deposit

Jin Xin1Yu Can 2   

  1. 1.Yuxi Mining Co.,Ltd.;2.Kunming Prospecting Design Institute of
    China Nonferrous Metals Industry Co.,Ltd.
  • Online:2020-06-25 Published:2021-09-14

摘要: 大红山铜矿床属火山喷气—搬运沉积—变质改造型矿床,矿化丰富,成因复杂。在系统收集矿区地质资料的基础上,结合野外调查工作、试验测试成果,对大红山铜矿区内的金、银矿化赋存状态和富集机制进行了研究。结果表明:①黄铜矿、黄铁矿等矿物中的独立金、银矿物是矿床中伴生金、银的主要产出形式;②曼岗河时期海底火山喷气—沉积作用奠定了金、银矿化基本格架,金、银矿化主要赋矿层位为曼岗河组第3岩性段;③I号矿带各矿段金、银矿化显示出与铜、铁矿化显著的正相关关系,其中I2、Ib、I3矿段中矿化强度最高;④金、银矿化层控特征显著,矿床演化过程严格受火山活动及岩相古地理控制,地层岩性、围岩蚀变、地球物理特征等共同组成了寻找大红山金、银矿化的有利标志。

Abstract: Dahongshan Copper Deposit is a volcanic exhalationtransport and depositionmetamorphic reformation type deposit,which characterized by rich mineralization and complicated genesis.Based on systematic collection of geological data of Dahongshan mining area,the occurrence and enrichment mechanism of goldsilver mineralization is obtained by combined with the field geological surveying and test results.The study results show that:①the independent goldsilver mineral are mainly occurred in chalcopyrite and pyrite;②the submarine volcanic exhalationsedimentation establish foundation for goldsilver mineralizaiton,in addition,the foldsilver mineralization is mainly occurred in third lithologic member of Manganghe Formation;③the significant positive correlation between the goldsilver mineralization and copperiron mineralization is presented,which have most mineralization internsity among I2,Ib and I3 oresection;④the goldsilver mineralization has the characteristic of stratabound,and the ore evolution strictly controlled by volcanic activity and lithogacies paleogeography,the formation lithology,wallrock alteration,geophysical characteristics can be regarded as the prospecting criteria for Dahongshan goldsilver mineralization.