摘要
本文通过大量的薄片及扫描电镜资料,描述了柳州白云岩中存在的多种形式的晶内微溶蚀特征,揭示了白云岩岩溶不同于灰岩岩溶的一些重要特点。
Based on a large amount of slices and photographs of electromicroscope scanning,this paper describes the microcorrosion features of Liuzhou dolomites. Some typical microcorrosion patterns have been presented, such as break-apart along a dominant set of cleavages, corrosion along two sets of cleavages, and corrosion along directional microcrack or irregular cracks on the surface of dolomite crystals. And they are possible the cause of dolomitic powder.
出处
《贵州科学》
1992年第2期8-16,共9页
Guizhou Science
