摘要
在浙江江山老虎山石灰岩中发现Parafusulina ,Verbeekina和Neoschwagerina等中二叠世蜓类 ,证明不是原来认为的石炭系石灰岩 ,而是二叠系石灰岩。
Fusulinidae of middle Permian was found,such as Parafusulina,Verbeekina and Neoschwagerina in limestone from Laohushan in Jiangshan, Zhejiang.It proves that it is limestone of Permian, instead of limestone of the Carboniferous period.
出处
《桂林工学院学报》
2001年第4期334-336,共3页
Journal of Guilin University of Technology
关键词
二叠纪
蜓类
地层
浙江
江山
灰岩
Permian
stratigraphy
layer
Jiangshan
Zhejiang
