摘要
湖南省道县小蓬江铅锌银矿床属高—中温岩浆热液充填交代型铅锌多金属矿床,分布于金鸡岭岩体西部内接触带中,受区域性断裂F1、F2的次级断裂带控制。岩体内接触带、控矿断裂及次级断裂带、云英岩化等蚀变、民采老窿等为矿床的找矿标志。矿区内北东向矿脉具沿走向、倾向延伸较稳定的特点,其深部具有扩大远景的可能。
The Xiaopengjiang lead-zinc-silver deposit in Daoxian county, Hunan province,is a high - middle temperature magmatic hydrothermal filling metasomatic lead-zinc polymetallic deposit. The ore veins are distributed in the contact zone of the western of the Jinjiling rock body, and are controlled by the secondary fault zone of the regional fault F1 and F2. The contact zone, ore controlling fault and secondary fault zone, alteration of greisenization , and the Mining old holeare the prospecting criteria for the deposit. The NE trending vein in the mining area has the characteristics of extending along the strike and tendencies, and its deep part has the possibility of expanding the prospect.
作者
康如华
许云舟
冯经平
刘大勇
李福顺
Kang Ruhua;Xu Yunzhou;Feng Jingping;Liu Dayong;Li Fushun(418 Geological Team,Bureau of Geology and Mineral Exploration and Development of Hunan Province,Loudi,Hunan,417000,China)
出处
《化工矿产地质》
CAS
2018年第4期193-197,共5页
Geology of Chemical Minerals
基金
国家矿产资源补偿费矿产勘查项目(项目编号:200401004)
关键词
铅锌银矿
地质特征
找矿远景
湖南省道县
Lead-zinc-silver deposit
Geological characteristics
Prospecting potential
Daoxian county
Hunan