摘要
白竹砂质高岭土矿位于武夷山北北东向隆起带西南侧与于山北东构造带的交接部位,处于珠兰埠岩体的边缘部位,属于花岗岩风化残积型砂质高岭土矿床。本文总结了矿床地质特征、矿床成因和矿化类型,分析矿区及周边找矿空间,认为矿区外同岩体面积广,深部瓷石找矿空间大。
The Baizhu sandy kaolin deposit is located at the junction of the southwest of Yushan NNE uplift belt and Yushan ne structural belt, it is located at the edge of Zhulanbu rock mass, it belongs to granite weathering residual sandy kaolin deposit.This paper studies the geological characteristics and genesis of the deposit, and mineralization types, analyze the prospecting space in and around the mining area, it is considered that the area of the same rock mass outside the mining area is wide, there is a large prospecting space for deep porcelain stone.
作者
钟远生
ZHONG Yuan-sheng(Nonferrous Geology Brigade of Jiangxi Geological Bureau,Ganzhou 341000,China)
出处
《中国非金属矿工业导刊》
2022年第5期38-41,共4页
China Non-Metallic Minerals industry
关键词
砂质高岭土矿
矿床地质特征
矿床成因
找矿潜力分析
sandy kaolin ore
geological characteristics
genesis of deposit
analysis of prospecting potential
