河北唐县齐家佐高岭土矿地质特征及成因探讨  

Geological Characteristics and Genesis of Qijiazuo Kaolin Deposit in Tang County, Hebei Province

作　　者：王政[1] 齐新国 王立考[1] 李博文 田贺[1] WANG Zheng;QI Xin-guo;WANG Li-kao;LI Bo-wen;TIAN He(Hebei Branch of China National Geological Exploration Center of Building Materials Industry,071051 Baoding,China)

机构地区：[1]中国建筑材料工业地质勘查中心河北总队,河北保定071051

出　　处：《中国非金属矿工业导刊》2022年第5期45-47,共3页China Non-Metallic Minerals industry

基　　金：地勘中心专项地质找矿项目“河北省唐县齐家佐—北山阳一带高岭土矿地质找矿”(编号:建地矿[2021]11号)。

摘　　要：唐县齐家佐高岭土矿赋存于燕山期石英钠长斑岩脉中,高岭土矿体呈脉状产出,层位稳定。矿石类型为高岭石石英型,矿石结构为斑状变余结构,块状构造。初步认为矿床成因类型属风化型高岭土矿床。The Qijiazuo Kaolin mine in Tang County is deposited in the quartz sodium long porphyry veins of the Yanshan period, and the Kaolin ore body is vein-like and stable. The ore type is Kaolin quartz type, and the ore structure is a spotted residual structure and a block structure. It is preliminarily believed that the genesis type of the deposit is a weathered Kaolin deposit.

关 键 词：高岭土 地质特征 成因探讨 齐家佐 

分 类 号：P619.232[天文地球—矿床学]