韶关大旺山矿区石灰岩矿矿床地质特征及成因分析  

GEOLOGICAL CHARACTERISTICS AND GENETIC ANALYSIS OF LIMESTONE DEPOSIT IN THE DAWANGSHAN MINING AREA,SHAOGUAN

作　　者：李静华 LI Jing-hua(Team 932,Guangdong Bureau of Nonferrous Geology,Shaoguan 512026)

机构地区：[1]广东省有色金属地质局九三二队,广东韶关512026

出　　处：《云南地质》2024年第3期397-402,共6页Yunnan Geology

摘　　要：大旺山矿区水泥用、建筑用石灰岩矿赋存于泥盆系天子岭组灰岩中。矿床成因为浅海相碳酸盐岩沉积矿床。水泥用和建筑用石灰岩均为大型矿床。矿体分布连续,矿石质量较好,矿山开发可带来良好的社会效益及经济效益。The limestone deposits used for cement and construction in the Dawangshan mining area are located in limestones ofthe Devonian Tianziling Formation.The deposits were formed bysediment of early Carboniferous shallow marine carbonate.Limestone deposits of cement andconstruction are both large in scale.The distribution of ore bodies is continuous,withgood ore quality.Mine development could bring good social and economic benefits.

关 键 词：水泥用灰岩 建筑用灰岩 地质特征 地质成因 大旺山矿区 广东韶关 

分 类 号：P619.225[天文地球—矿床学]