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作 者:刘必政[1] 张继林[2] 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)
机构地区:[1]中国黄金集团资源有限公司 [2]中国黄金集团有限公司 [3]山东烟台鑫泰黄金矿业有限责任公司 [4]北京金有地质勘查有限责任公司
出 处:《黄金》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)
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.
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
分 类 号:TD15[矿业工程—矿山地质测量] P618.51[天文地球—矿床学]
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