摘要
本文论述了干旱气候区硫化矿床氧化带的典型特征。氧化物种类繁多,颜色鲜艳,形态多样。垂直分带明显,各亚带均有不同程度的发育,亚带之间为渐变关系,笔者认为该氧化带形成时代应为第三纪末,第四纪初。
The oxidized ore zone of the sulfide deposit discussed here has typical pheatures of oxidation in high aridity environment. A big variety of oxide rhenerals are distributed in a certain regulation, displaying an obvious vertical zoning. The gossan subzone is well developed and the boundaries between subzones are continuous. It is believed that the oxidation process was developed in Tertiary-Quaternary.
出处
《矿物岩石》
CAS
CSCD
1989年第2期73-80,共8页
Mineralogy and Petrology
