摘要
黔东注溪钒矿含矿岩系为跨震旦-寒武系留茶坡组及下寒武统九门冲组第一段。通过对含矿岩系标志层的初步研究和对比分析,确定该区钒矿化地段一般分别分布于该标志层之上、下10-15m地层厚度范围内,这一特征为该区及其它地区钒矿找矿提供了一定的参考。
Vanadium-bearing rock series in Zhuxi, east Guizhou is the Sinian-Cambrian Liuchapo Formation and the First Member of the Lower Cambrian Jiumenchong Formation. Study and correlation of key bed of the Vanadium-bearing rock series indicate that V-bearing mineralization occurs in the limits of 10-15 m above and below the key bed.
出处
《四川地质学报》
2015年第1期76-79,共4页
Acta Geologica Sichuan
关键词
钒矿
标志层
对比分析
黔东注溪
Vanadium ore
key be
correlation
Zhuxi
east Guizhou
