新疆乌恰县沙热拉重晶石矿地质特征及矿床成因浅析
Geological Characteristics and Genesis of Sharela Barite Deposit in Ulugqat County,Xinjiang
李晓亚 1刘星旺 2王凡 2赵寒2
作者信息
- 1. 中化地质矿山总局,北京 100013
- 2. 中化地质矿山总局地质研究院,北京 100013
- 折叠
摘要
本文主要通过对沙热拉重晶石矿床地质特征和矿石特征的分析研究,探讨了重晶石矿床成因,总结了找矿标志.沙热拉重晶石矿床赋存于中泥盆统托格买提组,属低温热液脉型矿床.地层、构造控矿作用明显,中泥盆统托格买提组地层,断裂、破碎带等可作为找矿标志,对今后区域上同类矿床的找矿工作具有一定的指导意义.
Abstract
This paper mainly analyzes the geological characteristics and the mineral characteristics of the Sharela barite deposit,discusses the genesis of the barite deposit,and summarizes the prospecting indicators.The Sharela barite deposit occurs in middle Devonian Tuogemaiti Formation.The deposit belongs to low temperature hydrothermal vein type deposit.Middle Devonian Tuogemaiti Formation,fracture,crush belt are clues for prespecting.This pape can provide reference for the exploration of similar barite deposits in the region.
关键词
重晶石/矿床特征/矿床成因/乌恰县Key words
barite/deposit characteristics/genesis of deposit/Ulugqat county引用本文复制引用
基金项目
中化地质矿山总局化工地质科技项目(ZHDK202203)
出版年
2024
国家科技期刊平台
NSTL
维普
万方数据