摘要
分析了浙西和浙北二叠纪含煤岩系的地层序列和沉积特征，认为应属于同一盆地的沉积。与本文作者详细工作过的福建童子岩组进行比较。
The stratigraphic sequence and sedimentary environment of Permian coal bearing strata in western and northern Zhejiang Province are analyzed,it is believed that both bolong to the sediment in a same basin.The comparison with the Tongziyan Formation in Fujian Province,which was studied in detaits by the authors,is carried out,and the similarities in both sedimentary and coal accumulated regularities are pointed out.
出处
《煤田地质与勘探》
CAS
CSCD
北大核心
1997年第1期1-5,共5页
Coal Geology & Exploration
基金
国家自然科学基金
