摘要
通过贵州余庆小乌江钒矿地质背景、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-重结晶-氧化再沉积型矿床,该区寒武纪早期为海礁相相对缺氧的酸性环境。
Based on the study on thegeological background and orebody characteristics of Xiaowujiang vanadium deposit in Yuqing, Guizhou province, the metallogenic geological environment is comprehensively analyzed, and it is concluded that this deposit is of submarine hydrothermal exhalative sedimentation-recrystallization-oxidation resedimentation type.The early Cambrian is an acidic environment in which the reef is relatively anoxic.
作者
杨仕江
Yang Shijiang(The 3rd Team of Guizhou Nonferrous Metals and Nuclear Industry Geological Exploration Bureau, Zunyi 563000,China)
出处
《有色金属设计》
2018年第1期73-75,共3页
Nonferrous Metals Design
关键词
小乌江
钒矿
成矿环境
海底热液喷流
重结晶
缺氧酸性环境
Xiaowujiang
Vanadium ore
Metallogenic environment
Submarine hydrothermal exhalation
Reerystallization
Anoxic acid environment
