摘要
通过对济阳坳陷古近纪咸化层段源岩的饱和烃色谱质谱分析发现,沙河街组一段、沙三段和沙四段上亚段源岩中发育了可以指示海侵发生的甲藻甾烷和C31甾烷分子化石,并且C31甾烷通常出现在水体盐度更高、海侵程度更大的环境中,从而推测三个层段的咸化与海相关。
The study on chromatography mass analysis of saturated hydrocarbons in Paleogene saline formation of Jiyang Depression shows that dinosterane and C31 sterane developed in source rocks of the 1 s, member( Es, ), the 3^rd member( Es3 ) and upper the 4'h member( Es^U ) of Shahejie Formation, these molecular fossils are marks of marine transgression, moreover C3, sterane denotes that the formation is influenced more by sea water, therefore salinity of 3 members related to marine transgression.
出处
《沉积学报》
CAS
CSCD
北大核心
2008年第4期683-687,共5页
Acta Sedimentologica Sinica
基金
国家科技攻关项目(2003BA613A-02)资助
关键词
济阳坳陷
古近纪
分子化石
甲藻甾烷
C31甾烷
Jiyang Depression, Paleogene, molecular fossil, dinosterane, C31 sterane