摘要
本文研究了鄂西地区上二叠统吴家坪阶牙形石特征后,由上而下建立两个牙形石化石带:Neogondolella orientalis 带;N.leveni-N.liangshanensis 带,分别代表吴家坪阶的上部和下部,可与华南及国外有关地区对比。
Studied Wujiaping stage conodonts collected from Western Hubei,two conodontzones are established in descending order as follows:Neogondolella orientalis zone;Neogon-dolella leveni-N,liangshanensis zone.They represent respectively the upper and lower partsof the Wujiaping stage and could correlate with the eguivalent strata in South China andabroad.
出处
《石油与天然气地质》
EI
CAS
CSCD
北大核心
1993年第4期310-315,共6页
Oil & Gas Geology
