摘要
纳米比亚卡里比布矿区饰面大理岩矿赋存于寒武-奥陶纪哈考斯统地层中,经区域变质作用、热接触变质作用形成,岩性以白色、灰绿色大理岩为主,矿体呈层状分布,矿石质量、装饰性能较好,各项物理—力学性能指标满足规范要求,是优质的饰面石材材料,具有良好的开发利用前景。
The decorative marble mine in Kalibib mining area in Namibia is located in Cambrian - Ordovician Hakkaus strata and formed by regional metamorphism and pyrometamorphism. The lithology is mainly white and gray-green marble, Ore bodies are distributed in layers. Its ore quality and decorative performance are good, and various physical and mechanical performance indexes meet the specification requirements. It is a high-quality decorative stone material, and have good prospects for development and utilization.
作者
张燕挥
ZHANG Yanhui(Shandong Geophysical and Geochemical exploration institute, Jinan 250013, China)
出处
《四川有色金属》
2019年第1期53-56,共4页
Sichuan Nonferrous Metals
关键词
饰面大理岩
矿床地质特征
矿床成因
纳米比亚
Decorative marble
geological characteristics of ore deposits
genesis of deposit
Namibia
