摘要
通过贵州遵义庙子湾钼镍矿地质背景、矿体特征研究,对成矿地质环境进行综合分析,得出该矿床类型为海底热液喷流沉积型矿床,该区寒武纪早期为台地边缘缓坡相的酸性还原环境。
Through the study of the geological background and ore characteristics of Mo Ni ore in the temple of the Zunyi, Guizhou, the metallogenic geological environment is synthetically analyzed. It is concluded that the deposit type is the submarine hydrothermal jet sedimentary deposit, and the Early Cambrian period is an acidic reduction environment for the gentle slope facies of the platform edge.
作者
杨仕江
YANG Shi-jiang(The three general team of Guizhou nonferrous metals and Nuclear Industry Geological Prospecting Bureau, Zunyi 563000,Chin)
出处
《世界有色金属》
2018年第5期136-137,共2页
World Nonferrous Metals
关键词
庙子湾
钼镍矿
成矿环境
海底热液喷流
酸性还原环境
Miaozi Bay
molybdenum nickel ore
metallogenic environment
hydrothermal exhalation
acid reducing environment
