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湘中杏枫山金矿的磁黄铁矿矿物学研究

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杏枫山金矿位于湘中白马山—龙山—紫云山金矿带的西段,是湘中地区最重要的金矿之一,属于典型的石英细脉型金矿.杏枫山金矿赋存于高涧群岩门寨组的砂质板岩中,矿体主要产于NW向脆性剪切条带中,由密集的石英细脉组成;金属矿物主要为毒砂、磁黄铁矿和黄铁矿,脉石矿物主要为石英、方解石.文章拟对杏枫山矿区磁黄铁矿进行矿物学研究,对围岩板岩与矿体石英细脉中的磁黄铁矿进行结构分析,这对推动该矿选冶流程优化,有显著的意义.
Study on Pyrrhotite Mineralogy of Xinfengshan Gold Deposit in Longhui,Hunan Province
The Xingfengshan gold deposit,one of the most important gold deposits in central Hunan,is located in the western part of the Shirama-yama-Long Son-Ziyunshan gold belt in central Hunan and belongs to a typical quartz veiulet type gold deposit.The Xingfengshan gold deposit occurs in the sandy slate of the Yanmenzhai Formation of the Gaojian Group.The orebody mainly occurs in the NW-trending brittle shear zone and is composed of dense quartz veins.The metal minerals are mainly arsenopyrite,pyrrhotite and pyrite,and the gangue minerals are mainly quartz and calcite.In this paper,the mineralogy of pyrrhotite in Xingfengshan mining area is studied,and the structure of pyrrhotite in wall rock slate and quartz vein is analyzed,which is great significance to promote the optimization of the ore dressing and smelting process.

pyrrhotitestructural analysisquartz veinlet type gold depositXinfengshan gold deposit

肖鸿杰、刘宏钦

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金杏矿业有限公司,湖南 隆回 422000

磁黄铁矿 结构分析 石英细脉型金矿 杏枫山金矿

2024

湖南有色金属
湖南有色金属研究院,湖南有色金属学会

湖南有色金属

影响因子:0.393
ISSN:1003-5540
年,卷(期):2024.40(6)