摘要
本文研究了华北聚煤区１３条剖面的孢粉资料，划分了七个组合带，建立了石炭、二叠纪孢粉生物地层序列。根据孢粉组合发育特征的分析，认为石炭、二叠系界线应置于第Ⅱ组合带与第Ⅲ组合带之间。
After studied sporopollen inforniation from 13 sections in North China coal ac-cumulation area,a Permo-Carboniferous sporopollen biostratigraphic succession has beenworked out by the author.According to the development features of sporopollen assemblages,the Permo-Car-boniferous boundary was put between the 2nd assemblage zone and the 3rd assemblage zone.
出处
《中国煤田地质》
1994年第4期7-15,共9页
Coal Geology of China
关键词
石炭纪
二叠纪
孢粉
生物地层
煤系
North China coal accumulation area
Permo-Carboniferous
spporopollen
biostratigraphy
