贺州里松矿区大狼冲钾长石矿地质特征及矿床成因  

Geological Characteristics and Genesis of Daluchong Potassium Feldspar Deposit in Lisong Mining Area,Hezhou

作　　者：冼道学 李旭成[1,2] 李言复 杨文海 杨琨 XIAN Dao-xue;LI Xu-cheng;LI Yan-fu;YANG Wen-hai;YANG Kun(Guangxi Geological Exploration Institute of China Metallurgical Geology Bureau,Nanning 530000,China;Institute of Mineral Research of China Metallurgical Geology Bureau,Beijing 101300,China;Nanning Sandie Geological Resources Development Co.,Ltd.,Nanning 530000,China)

机构地区：[1]中国冶金地质总局广西地质勘查院,广西南宁530000 [2]中国冶金地质总局矿产资源研究院,北京101300 [3]南宁三叠地质资源开发有限责任公司,广西南宁530000

出　　处：《中国非金属矿工业导刊》2023年第3期28-30,42,共4页China Non-Metallic Minerals industry

摘　　要：里松矿区钾长石矿赋存于花岗岩风化壳中,属风化残余矿床。文章通过总结贺州市里松矿区大狼冲钾长石矿的矿床特征、矿体特征以及矿石质量,分析矿床成因以及控矿因素,旨在为该区域寻找同类钾长石矿提供帮助。The potassium feldspar deposit in Lishong Mining area occurs in granite weathering crust and belongs to weathering residual deposit.This paper summarizes the deposit characteristics,ore body characteristics and ore quality of the potassium feldspar ore deposit in Babulisong mining area,Hezhou,analyzes the deposit genesis and ore control factors,aiming to provide help for the search for similar potassium feldspar ore in this area.

关 键 词：钾长石矿 地质特征 矿床成因 大狼冲 贺州 

分 类 号：P619.235[天文地球—矿床学]