摘要
通过对南好地区南兵 -公井岭剖面志留纪足赛岭组上部所发现的Favocites动物群的埋藏特征、地层层序的初步研究和对该区志留系生物地层的综合分析 ,并与川北陕南、长江三峡等地相关地层对比 。
Favocites fauna is first discovered in the upper part of Zhusailing Formation in Nanhao area of Hainan province. Based on systematical contrastive study of Favocites fauna on burying characteristics,stratigraphic sequence and Silurian biostratigraphy with those in northeast Sichuan,south Shanxi,Yangtze Gorges area, it is concluded that the upper part of the Silurian Zhusailing Formation belong to Late Telychian Stage of Landovery Epoch.
出处
《华南地质与矿产》
CAS
2000年第4期23-27,共5页
Geology and Mineral Resources of South China
基金
1:2 5万乐东县幅 (E49C 0 0 2 0 0 1)
陵水县幅 (E49C 0 0 2 0 0 2 )区域地质调查项目成果
