ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西藏隆子县扎西康锌多金属矿床矿石组构研究及成因探讨
  
关键词:Zhaxikang  Zn-polimetallic deposit  ore fabric  metallogenesis epoch  metallogenesis stage  genesis
基金项目:国家973项目(编号: 2011CB403103);公益性行业科研专项(编号: 201011013-3)
作者单位E-mail
王艺云 成都理工大学 wangyiyun1988@163.com 
唐菊兴 成都理工大学中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室  
郑文宝 中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室  
林彬 成都理工大学  
冷秋锋 成都理工大学  
陈伟 成都理工大学  
丁帅 成都理工大学  
宋俊龙 成都理工大学  
徐云峰 成都理工大学  
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摘要:
A Tentative Discussion on Ore Fabric and Genesis of the Zhaxikang Zn-polymetallic Deposit, Lhunze County, Tibet
      Based on detailed drilling geological record and microscopic identification, the authors conducted a systematic study of the ore fabric characteristics of the Zhaxikang zinc-polymetallic deposit. In the mining area, the main ore structures are blocky, stockwork, disseminated, brecciated, geode and druse ones, formed by typical filling and metasomatism. The ore textures were formed mainly by crystallization and metasomatism, and subordinately by the influence of the pressure and the solid solution. Tectonism and mineralization of this mining area are of multi-stage and complex characteristics, and thus the textures formed by metasomatism are most common and of various types. Based on the research result of the ore fabric, combined with previous studies, the authors roughly divided the metallogenic periods into diagenesis, middle to low-temperature hydrothermal mineralization and supergene oxidation, with the low-temperature hydrothermal mineralization period being the most important metallogenetic period in this deposit. According to the features of mineral assemblages, six stages of mineralization were recognized, i.e., pyrite-quartz-calcite stage, sphalerite-pyrite-galena-arsenopyrite-iron rhodochrosite stage, galena-sphalerite- sulfosalt minerals stage, quartz-calcite-stibnite stage, quartz-calcite stage and oxidized minerals stage. It is held that the Zhaxikang zinc polymetallic deposit is a middle to low-temperature hydrothermal deposit, formed by filling and metasomatism and controlled by tectonic-magmatic activity.
WANG Yi-yun,TANG Ju-xing,ZHENG Wen-bao,LIN Bin,LENG Qiu-feng,CHEN Wei,DING Shuai,SONG Jun-long,XU Yun-feng.2012.A Tentative Discussion on Ore Fabric and Genesis of the Zhaxikang Zn-polymetallic Deposit, Lhunze County, Tibet[J].Acta Geoscientica Sinica,33(4):681-692.
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