浙江江山老虎山灰岩时代的新认识  

Realization of the limestone period from Laohushan in Jiangshan of Zhejiang

作　　者：李罗照[1] 韩乃仁[2] 

机构地区：[1]江汉石油学院,湖北荆州434102 [2]桂林工学院资源与环境工程系,广西桂林541004

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

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.

关 键 词：二叠纪 蜓类 地层 浙江 江山 灰岩 

分 类 号：P534.46[天文地球—古生物学与地层学]