摘要
湖南黄沙坪铅锌矿区南部铁钨钼铋(锡)多金属矿床是湘南多金属成矿带的重要矿床之一。文章通过综合研究地层、构造、岩浆岩及夕卡岩的特征,论述了矿床的主要控矿因素;从矿体类型、矿石类型及矿物组成特点、矿化与蚀变分带性、成矿期次及成矿温度研究,论述了矿床的成因与成矿规律;通过综合分析,提出了该区进一步找矿的方向。
The Fe -W -Mo- Bi - （Sn） polymetallic deposit in the southern part of the Huangshaping lead -zinc mine district is one of the important deposits in the Hunan polymetallic metallogenic belt, Hunan Province, China. In this paper, on the basis of comprehensive studies on the characteristics of the stratigraphy, structure, magmatic rock and skarn, the main ore - controlling factors are analyzed; On the basis of studies on orebody type, ore type, and mineral assemblages, mineralization and alteration zonation, metallization periods and ore -forming temperature, the ore deposit genesis and mineralization regularity are discussed. Finally, the target is given for further exploration.
出处
《矿产勘查》
2010年第4期323-333,共11页
Mineral Exploration
关键词
黄沙坪
铁钨钼铋(锡)多金属
夕卡岩
矿体类型
控矿因素
Huangshaping
Fe- W- Mo- Bi（ -Sn）
polymetallic
skarn
orebody type
ore-controlling factor
