摘要
四川火烧云铅锌矿床位于区域龙门山大巴山台缘坳陷、四川台坳及扬子台坳的交接部位,综合矿床地质特征、矿体特征,矿石矿物结构构造、矿体产状及围岩蚀变特征,火烧云铅锌矿床应归属于受构造控制的热液型铅锌矿床,成矿来源为震旦系灯影组碳酸盐地层。
The Huoshaoyun lead-zinc deposit in Sichuan is located at the junction of Dabashan platform margin depression,Sichuan platform depression and Yangzitai depression in Longmenshan region.It synthesizes the geological characteristics,ore body characteristics,ore mineral structure,ore body occurrence and wall rock alteration characteristics.The Huoshaoyun lead-zinc deposit should belong to the hydrothermal lead-zinc deposit controlled by structure,and the ore-forming source is Sinian Dengying Formation carbon.Salt formation.
作者
胡文辉
邱颖盛
沈寅
HU Wen-hui;QIU Ying-sheng;SHEN Yin(Jiangxi Geological and Mineral Resources Exploration and Development Co.,Ltd.,Nanchang 330000,China;Geochemical Exploration Team of Sichuan Geological and Mineral Exploration and Development Bureau,Deyang 618000,China)
出处
《世界有色金属》
2019年第18期278-278,280,共2页
World Nonferrous Metals
关键词
四川
铅锌矿床
地质特征
矿床成因
Sichuan
lead-zinc deposits
geological characteristics
genesis of deposits
