摘要
龙口-土堆金矿区位于胶莱盆地东北缘,控制矿体主要赋存在-400 m标高以上的浅部,矿体规模相对较小、不连续,而其周边的辽上、西涝口金矿区在-500 m标高以下均实现了找矿突破,且矿体规模厚大。通过对比龙口-土堆金矿床与辽上、西涝口金矿床的地质特征,并结合区域成矿背景,认为龙口-土堆金矿区深部具有较大的成矿潜力,且深部找矿应以牧牛山岩体与荆山群地层接触带为主。
The Longkou-Tudui Gold District is located in the northeast of the Jiaolai Basin. The district controlled ore bodies mainly spread shallower than the-400 m elevation and are small-scale and discontinuous. However,exploration breakthroughs have been made in the adjacent Liaoshang and Xilaokou gold districts below the-500 m elevation and the ore bodies are thick and large-scale. By comparing the geological characteristics of the Longkou-Tudui Gold Deposit and the Liaoshang and Xilaokou gold deposits and based on regional metallogenic settings,it is indicated that there are great resource potentials in the deep levels of Longkou-Tudui Gold District and the deep prospecting should be carried out on the contact zone of Muniushan rock mass and Jingshan group strata.
作者
刘必政
张继林
冯波
魏兴亮
刘彦兵
秦连元
Liu Bizheng;Zhang Jilin;Feng Bo;Wei Xingliang;Liu Yanbing;Qin Lianyuan(China Gold Group Resources Co. ,Ltd.;China National Gold Group Co. ,Ltd.;Shandong Yantai Xintai Gold Mining Industry Co. ,Ltd.;Beijing Jinyou Geological Exploration Limited Liability Company)
出处
《黄金》
CAS
2019年第10期10-13,共4页
Gold
基金
中国黄金集团公司科研项目(ZJ-KY/2015-ZY-02)
关键词
龙口-土堆金矿区
胶莱盆地
胶东金矿集区
辽上金矿床
西涝口金矿床
成矿潜力
找矿方向
Longkou-Tudui Gold District
Jiaolai Basin
Jiaodong high ore concentration district
Liaoshang Gold Deposit
Xilaokou Gold Deposit
metallogenic potential
prospecting indication