摘要
兴城市镇南山地区位于青龙-葫芦岛近东西向大断裂东段，碱厂岩体内部，区内断裂构造发育，岩浆活动强烈。矿（化）体赋存于石英砂岩原生节理中，矿化类型主要为热液充填含钳石英脉型。本文主要根据近两年来对该区进行普查工作的地质找矿资料综合研究分析的基础上，以及结合区域上的地质成矿背景条件，对本地区内的钼成矿地质条件及深部找矿前景进行了初步探讨。
Zhennanshan Area of Xingcheng, is located in the East part of the Qinglong--Huludao East-- West Fracture, inside the Jianchang rock mess. The fracture structure development in this areas with in- tensive magmatic activity. The ore body is hosted in the original joint of quartz sandstones, and the miner- alization is mainly hydrothermal--filled Mo quartz vein type. In this paper, according to prospecting data of geological prospecting in the area in the last two years , on the basis of comprehensive analysis, and combined with the geological and metallogenic background conditions of the region, the preliminary discus- sion on local area of molybdenum ore--forming geological conditions and deep prospecting prospect has carried on.
出处
《有色矿冶》
2013年第5期1-3,共3页
Non-Ferrous Mining and Metallurgy
关键词
镇南山
钼矿化
成矿地质条件
深部找矿前景
Zhennanshan
Mo mineralization
geographic condiions for mineralization
deep exploration
