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Formation Conditions of Deposits of the Gold-Quartz Formation in the Muya Zone (Northern Transbaikal Region)

机译:穆亚地区(北贝加尔湖地区)金-石英层金矿床的形成条件

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摘要

The Muya structural zone, one of the regions with a high potential of gold mineralization, incorporates more than 300 gold occurrences and deposits. Ore occurrences of the gold-quartz formation are most widespread in this region (Fig. 1). Deposits of the gold-quartz formation in the Muya zone are primarily associated with island-arc volcano-plutonic complexes. Gold ore occurrences are confined to cratonic, turbidite, and island-arc terranes. However, many issues about their distribution and for- mation constraints, as well as the relationships between disseminated and vein types of gold-sulfide mineralization, are insufficiently studied.
机译:Muya构造区是金矿化潜力高的地区之一,其中包含300多个金矿和矿床。金石英形成的矿石发生在该地区最为普遍(图1)。穆亚地区金-石英形成的沉积物主要与岛弧火山-火山岩复合体有关。金矿的发生局限于克拉通,浊积和岛弧地层。然而,关于硫化金矿化的分布和形态约束以及散布和脉型之间的关系的许多问题尚未得到充分研究。

著录项

  • 来源
    《Doklady Earth Sciences》 |2006年第8期|p.1171-1173|共3页
  • 作者

    B. N. Abramov;

  • 作者单位

    Chita Institute of Natural Resources, Siberian Division, Rssian Academy of Sciences, ul. Butina 26, Chita, 672090 Russia;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 天文学、地球科学;
  • 关键词

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