重庆秀山地区大塘坡式锰矿典型矿床成矿要素及成矿模式分析——以重庆市秀山县鱼泉锰矿床为例  

Analysis on the Metallogenic Essential Factor and Metallogenic Model of Datangpo-type Typical Manganese Deposit in Xiushan District,Chongqing

作　　者：蔡柯柯 王万良 张林[2] 郭亮 齐玲玲 CAI Keke WANG Wanliang ZHANG Lin GUO Liang QI Lingling(607 Geological Team of Chongqing Bureau of Geology and Minerals Exolortion, Chongqing 400054, China Hunan Planning Institute of Land and Resources, Changsha 410007, China)

机构地区：[1]重庆市地质矿产勘查开发局607地质队,重庆610059 [2]湖南省地质科学研究院,湖南长沙410007

出　　处：《四川有色金属》2017年第2期35-38,共4页Sichuan Nonferrous Metals

摘　　要：秀山县鱼泉锰矿床位于秀山县,属武陵山构造区。笔者通过研究矿床的地质特征,从地层、构造、岩相古地理、矿体形态、矿石特征等方面分析了矿床的成矿要素,根据矿床经历的地质作用,以及矿物质来源认为矿床为热水喷流与海水混合沉积型矿床,并在此基础上总结出了重庆市秀山县鱼泉锰矿床成矿模式。Yuquan manganese deposit locates in XiuShan County, belongs to the Wuling mountain tectonic region. Through the study of geological characteristics of ore deposit, the author analyzed the metallogenic essential factor of the deposit from the aspects of formation, structure, lithofacies paleogeography, the morphology of ore body and the ore characteristics, etc,. According to the research on the geological process and ore matter source, it is believed that the deposit is hydrothermal exhalative and seawater mixing sedimentary deposit, and then summarized the metallogenic model of the Yuquan manganese deposit, XiuShan County, Chongqing.

关 键 词：重庆 鱼泉锰矿床 成矿要素 成矿模式 

分 类 号：P618[天文地球—矿床学]