img

QQ群聊

img

官方微信

高级检索

J4 ›› 2010, Vol. 18 ›› Issue (1): 22-26.

• 矿产勘查 • 上一篇    下一篇

甘肃金山、马泉金矿床对比研究

 姜启明, 鲁挑建   

  1. 甘肃工业职业技术学院,甘肃  天水   741025
  • 出版日期:2010-02-25 发布日期:2010-04-22
  • 基金资助:

    中央财政资助地质勘查项目(编号:2004-197)资助.

A Comparative Study of Gansu Jinshan and Maquan Gold Deposit

  1. Gansu Vocation & Technology Institute of Industry, Tianshui   741025,Gansu,China
  • Online:2010-02-25 Published:2010-04-22

摘要:

金山、马泉矿床定位于礼县—白云—山阳大断裂西段膨大、分支锐角夹持区,通过对矿床区域地质背景、地质特征、成因等要素的对比分析,认为矿床地质特征相似、成因相同或类似。金山、马泉金矿的金源很可能来自中石炭统;硫来自深部,可能由岩浆水提供;成矿热液水由大气降水与岩浆水、变质水混合而成;矿床是在中低温、弱酸性、弱氧化—还原介质、弱矿化度条件下形成的微细浸染型热液金矿床。这2个矿床应为同一个矿床,在以后的地质勘查中应统筹考虑(特别是2个矿床的结合部),扩大现有矿床规模。

Abstract:

Jinshan and Maquan gold deposits are located in Lixian-Baiyun-Shanyang deep fault between swollen west section and branch acute angle clamp area. According to the comparative study of regional geological setting,geological characteristics and metallogenic genesis,we think that it have similar geological characteristics and deposit genesis.Jinshan,Maquan gold resources is likely to come from the Carboniferous;sulfur come from depth,it may be caused by magmatic water;ore-forming hydrothermal water come from mixture of atmospheric precipitation and magmatic water, metamorphic water;deposits are micro-disseminated hydrothermal gold deposit formed in conditions of low-temperature,weak acid,weak oxidation-reduction medium,weak mineralization.It is thought that the two deposits should be one,and it require overall consideration for future geological survey(especially the joint of two deposits),and expand the current deposit scale.

No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!