石油与天然气地质 ›› 1983, Vol. 4 ›› Issue (1): 89-99.doi: 10.11743/ogg19830107

• 论文 • 上一篇    下一篇

冀中坳陷原油和生油岩中的甾烷和萜烷

张振才, 王忠然, 陈献忠, 曾宪章   

  1. 石油工业部华北石油勘探开发设计研究院
  • 收稿日期:1981-11-15 出版日期:1983-03-25 发布日期:2012-01-16

GONANES AND TERMNES FROM CRUDE OIL AND SOURCE ROCKS IN JIZHONG DEPRESSION

Zhang Zhencai, Wang Zhongran, Chen XianZhong, Zeng Xianzhang   

  1. Research Institute of Petroleum Exploration and Development, Huabei Petroleum Administration
  • Received:1981-11-15 Online:1983-03-25 Published:2012-01-16

摘要:

近十几年来,随着色谱-质谱-计算机联用技术的发展,各种生物标记物的研究成果,在石油勘探中得到越来越广泛的应用。其中,甾烷和三萜烷的研究,特别引人注目。 早在五十年代末,W.G.Meinschein等人就曾报道过在现代沉积物和原油中发现了甾烷和萜烷。1965年,A.L.Burlingame等人首先从美国西部始新统格林河页岩中,分离和鉴定出C27—C29甾烷和C30五环三萜烷。

Abstract:

Crude oils and source rocks in Raoyang and Beijing-Tianjin sags as well as in the east slope of Ningjin uplift of Jizhong(central Hebei)depression are compared by the parameters of gonane and terpane stereoisomers.It is shown in a preliminary way that oils in Sinian buried hills of Renqiu Oilfield might come from different sources around,i.e.from the 1st and 3rd members of Shahejie Formation (E3s);oils in Ordovician in the north slope of this field from Kongdian Formation (E2k)of Bacian sag;oils Beijing-Tianjin region primarily from the 4th member of Shahejie Formation and Kongdian Formation,whereas oils in the 3rd member of Shahejie Formation might come from insitu.Oils in the 4th member of Shahejie Formation in th east slope of Ningjin uplift still preserved clear marks of terpanes,though they were subjected to biological degradation,this implies that these oil might come from the saline 4th member of Shahejie Formation. Thermal evolution of source rocks in Jizhong depression is discussed with three gonane and terpane parameters,which can accurately reflect the threshold depth and the peak of oil generation.According to the abundance of gonanes and terpanes,as well as the amount of gammacerane in saturated hydrocarbons,the authors suggest that the organic matters in Raoyang sag is better than that in Beijing-Tianjin sag.