河北丰宁头道沟萤石矿地质特征及找矿方向  

Geological Characteristics and Prospecting Direction of the Toudaogou Fluorite Deposit in Fengning, Hebei Province

作　　者：王政[1] 齐新国 王立考[1] 李博文 李艳杰 WANG Zheng;QI Xin-guo;WANG Li-kao;LI Bo-wen;LI Yan-jie(HeBei Branch of China National Geological Exploration Center of Building Materials Industry,Baoding 071051,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4期12-14,共3页China Non-Metallic Minerals industry

基　　金：地勘中心专项地质找矿项目“河北省丰宁县头道沟一带萤石矿地质找矿”(编号:建材地勘科技发[2021]125号)。

摘　　要：丰宁头道沟一带萤石矿赋存于下白垩统张家口组火山碎屑岩中,共发现2个矿体,呈脉状产出。矿石类型属石英萤石型,矿石结构为粒状结构,块状构造,少量皮壳状构造及条带状构造。属于岩浆期后中—低温热液充填型脉状矿床,为构造—岩浆活动的产物。The fluorite ore in the Fengning Tou daogou area was deposited in the volcanic clastic rocks of the Zhangjiakou formation of the lower Cretaceous system, and a total of 2 ore bodies were found, which were vein-like. The ore type belongs to the quartz fluorite type, and the ore structure is a granular structure, a block structure, a small amount of shell structure and a strip structure. It belongs to the medium-low temperature hydrothermal filled veined mineral deposits after the magmatic period, and is the product of tectonic-magmatic activity.

关 键 词：头道沟萤石矿 构造中低温热液 找矿方向 

分 类 号：P619.215[天文地球—矿床学]