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首页   >    黄金地质

青海省那尔扎金矿床地质特征及控矿因素

  • 张俊海|马元林|赵伟|莫延强
  • 作者单位:
  • 青海省地质调查局|青海省地质调查局|青海省地质调查局|青海省地质调查局
  • 基金项目:

  • 青海省地质勘查基金项目(2017042129kc079)
  • 详细信息:

  • 作者简介:
  • 张俊海(1990—),男,青海民和人,工程师,硕士,从事矿产调查评价工作;西宁市城西区胜利路22 号地矿花园C座508室,青海省地质调查局,810001;E-mail:903183233@qq.com
  • 通讯作者:
  • isnull
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Geological characteristics and ore-controlling factors of Naerzha Gold Deposit,Qinghai Province

  • English Author:
  • Qinghai Geological Survey|Qinghai Geological Survey|Qinghai Geological Survey|Qinghai Geological Survey
  • Unit:
  • 摘要
  • 在线预览
  • 参考文献

摘要:

那尔扎金矿床位于东昆仑成矿带东段,矿区内已发现5条金矿化带,共圈定9条金矿体。通过分析成矿地质背景、矿区及矿床地质特征,进而探讨了控矿因素。分析表明:矿体主要赋存在上二叠统格曲组中,围岩蚀变主要有绢云母化、硅化、黄铁矿化、碳酸盐化、褐铁矿化、高岭土化、绿泥石化,其中硅化、黄铁矿化、褐铁矿化与成矿关系密切;断裂构造是主要控矿因素,矿化带和矿体主要受北西西向断裂构造控制。

关键词:

那尔扎金矿床;地质特征;控矿因素;断裂构造;青海省

Abstract:

Naerzha Gold Deposit is located at the east part of East Kunlun metallogenic belt.In the gold district,5 gold mineralization belts are discovered and 9 gold ore bodies are delineated.By analyzing ore-forming geologic settings,deposit and district geologic characteristics,ore-controlling factors are discussed.The analysis shows that the ore bodies mainly occur in Upper Permian Gequ Formation; surrounding rock alteration mainly includes sericitization,silicification,pyritization,carbonatization,limonitization,kaolinization and chloritization; and among them,silicification,pyritization and limonitization are closely related to mineralization; fault is the main orecontrolling factor; metallogenic belts and ore bodies are mainly controlled by NWW fault structure.

Keywords:

Naerzha Gold Deposit;geological characteristics;ore-controlling factors;fault structure;Qinghai Province