摘要
通过对二道沟钨钼矿区区域地质背景、成矿构造环境、成矿地质特征及矿化分布规律的综合研究,认为该区属于高温热液石英脉型钨钼矿床。通过对成因类型初步探索,为区内下一步地质找矿工作指明方向。
Based on the comprehensive study of regional and geological setting,metallogenic tectonic setting,geological mineralization characteristics and distribution regularity in the Erdaogou ore field,It is considered that the Erdaogou tungsten-molybdenum deposit belongs to the middle-high temperature quartz-vein type.According to preliminary study of the genetic type,this paper has pointed out the geological prospecting direction for the further work in the study area.
引文
[1]王泰山,鲁海峰,张尧,等.青海省格尔木二道沟白钨矿床地质特征初析[J].中国钨业,2016,31(4):14-20.
[2]青海省地质调查院.青海省格尔木市巴拉大才-小南川金钨多金属矿调查评价报告(2013—2015年)[R].2016.
[3]青海省地质调查院.青海省格尔木市昆仑河地区矿产远景调查地球化学普查报告[R].2012.
[4]青海省地质调查院.青海省昆仑河地区金多金属矿整装勘查找矿部署研究报告[R].2015.
[5]韦星林.我国近年钨矿勘查新发现及其启示[J].中国钨业.2016,31(3):1-7.