摘要
在云南的曲靖、盘溪和广西的桂林、阳朔地区，中、晚泥盆世的海相灰岩广泛分布，根据微相特征划分出１３种微相类型．它们代表５种不同的沉积环境。沉积环境的分异与当时的海底地形和海平面的升降密切相关。
Middle and late Devonian marine limestone is distributed extensively in Qujing .Panxi of Yunnan Province and in Guiling.Yangshuo of Guangxi Province.13 microfacies types.which represented 5 different sedimentary environ ments,were divided according to microfacies The differentiation of environment was interrelated closely withthe submarine morphology and changes of the sea level.
出处
《安徽地质》
1996年第3期24-29,87-88,共8页
Geology of Anhui
基金
国家教委留学基金
关键词
碳酸盐岩
微相
沉积环境
泥盆纪
云南
广西
calcium carbonate.microfacies,sedimentary environment.Devonian Period,Devonian Period.Yunnan.Guangxi
