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干旱区地理 ›› 1991, Vol. 14 ›› Issue (1): 38-41.doi: 10.13826/j.cnki.cn65-1103/x.1991.01.007

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阿尔泰山砂金矿物质来源初探

陈锡飞, 叶玮, 达吾勒   

  1. 中国科学院新疆地理研究所
  • 出版日期:1991-03-25 发布日期:2025-12-25
  • 基金资助:
    “阿尔泰山砂金矿沉积规律研究”课题

THE RESOURCES OF ALTAI GOLD-PLACERS

Chen Xifei, Ye Wei, Dawuel   

  1. Xinjiang Institute of Geography, Academia Sinica
  • Published:1991-03-25 Online:2025-12-25

摘要: 阿尔泰山砂金矿,分布广泛,开采历史悠久。但对砂金矿的物质来源缺乏系统的研究。本文从阿尔泰山的地质发展史、砂金矿的地质构造和成因机制等方面的探讨,认为阿尔泰山砂金矿有四种原生金源:低含金矿化带、原生金矿床、伴生金和含金地层。它们经过中、新生代长期风化剥蚀和富集,构成了砂金矿的物质来源。据目前已知情况,其中低含金矿化带是最主要的金源。

关键词: 阿尔泰山砂金矿, 低含金矿化带, 接触蚀变带, 破碎蚀变带, 区域蚀变带

Abstract: Altai gold-placers are very famous for their high grade and wide distribution. But few people have investigated the material origin of gold-placers systematically. The study of geo-logical history of the Altai Mountain and geological feature and forming mechanism of gold-placers shows that Altai gold-placers have four original resources. That is, the poor gold-containing mineralized belts, the gold-deposits, the gold-containing metallic ores and the goldbearing rocks. Among them, the poor gold-containing mineralized belts are the main resources of Altai gold-placers