摘要
湘南二叠系碎屑岩、泥质岩、碳酸盐岩和硅质岩,具有富集Sb、Mo、Cu、Pb、Zn、Sn、Ag、Bi等元素的特征,是有利赋矿层位,其沉积物源具有陆源碎屑与火山物质混合的特点,当冲组硅质岩为非正常海相沉积成因。
Rocks of Permian System including sandstone,argillite,carbonate rocks and silicilith are relatively rich in Sb,Mo,Cu,Ph,Zn,Sn,Ag and Bi,and are also the favourable strata for ore-storing.Sediments in these rocks have the mixed proprerties of terrigenous fragments and volcanic materials,Silicilith of Dangcong Formation is of anormal marine origin.
出处
《湖南地质》
1996年第1期19-21,共3页
Hunan Geology
关键词
二叠纪
岩石
地球化学
物源指示
southern Hunan,Permian System,distribution of elements,provenance of sediments