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云南都龙锡锌多金属矿床闪锌矿主微量元素特征及其成矿指示意义

Main Element and Trace Element Characteristics and Metallogenic Indication of Sphalerite in Dulong Sn-Zn Polymetallic Deposit, Yunnan Province

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【作者】 尹文杰成永生吴湘滨

【Author】 YIN Wen-jie;CHENG Yong-sheng;WU Xiang-bin;School of Earth Science and Information Physics,Central South University;Key Laboratory of Nonferrous Metallogenic Prediction and Geological Environment Monitoring,Ministry of Education,Central South University;Hunan Key Laboratory of Nonferrous Resources and Geological Hazard Exploration;

【机构】 中南大学地球科学与信息物理学院中南大学有色金属成矿预测与地质环境监测教育部重点实验室有色资源与地质灾害探查湖南省重点实验室

【摘要】 都龙锡锌多金属矿床位于云南省文山州马关县的东南部,是老君山成矿区内最为重要的锡锌矿床之一,是我国继云南个旧锡矿床和广西大厂锡矿床后的第三大锡矿床。在研究区域地质特征和矿床地质特征的基础上,通过对都龙锡锌多金属矿床的闪锌矿电子探针分析得出,矿床中的Zn元素置换了Fe元素,矽卡岩的形成温度逐渐降低,并且通过Fe元素和Zn元素的含量能够得出矿床的温度是由中温到中低温。

【Abstract】 Dulong Sn-Zn Polymetallic Deposit is located in the southeast of Manguan County, Wenshan prefecture, Yunnan Province. It is one of the most important Sn-Zn polymetallic deposit in Laojunshan metallogenic area and the third largest tin deposit in China after Gejiu Sn Deposit in Yunnan Province and Dachang Sn Deposit in Guangxi Province. On the basis of geological features and ore deposit geology, through the analysis of Dulong Sn-Zn Polymetallic Deposit with the phalerite electron microprobe, it shows that the Zn deposit element displaces Fe element, and the formation of skarn temperature gradually decreases; and it can lead to that the temperature of the deposit changes from the medium temperature to low temperature through the contents of Fe element and Zn element.

  • 【分类号】P618.2
  • 【下载频次】131
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