摘要
通过对三都县苗龙锑矿产出特征、成矿期次、成矿时代、成矿物理化学特征等分析,认为区内锑矿成因属浅成中—低温热液型矿床,进一步划分为泥灰岩中热液充填交代石英脉型锑矿床,并对区内找矿标志进行总结。
Based on the analysis of the occurrence characteristics, metallogenic stages, metallogenic epochs and physicochemical characteristics of the Miaolong antimony deposit in Sandu County, it is concluded that the genesis of the antimony deposit in this area belongs to the epithermal-mesothermal type deposit, which is further divided into the quartz vein type antimony deposit with hydrothermal filling metasomatism in marl, and the prospecting criteria in this area are summarized.
引文
[1]陶平,陈建书,等.关于贵州省成矿区带初步划分方案[J].贵州地质,2018,35(3):171-180.
[2]贵州省地质矿产局一0四地质大队.贵州省三都县苗龙金矿床详查地质报告[R].1990.
[3]李红阳,高振敏,等.贵州丹寨卡林型金矿床地球化学特征[J].地质科学,2002,37(1):1-7.
[4]贵州省地矿局地质科研所.贵州锑矿成矿条件富集规律及找矿方向研究[R].1989.