石油学报 ›› 1981, Vol. 2 ›› Issue (3): 103-106.DOI: 10.7623/syxb198103012

• 学术讨论 • 上一篇    

松辽盆地主要生油期及生油门限温度(深度)的探讨

方祖康   

  1. 大庆石油学院
  • 收稿日期:1980-04-21 出版日期:1981-07-25 发布日期:2013-07-08

DISCUSSIONS ON THE MAIN PERIODS AND THRESHOLD TEMPERATURE(DEPTH)OF OIL GENERATION IN THE SONGLIAO BASIN

Fang Zukang   

  1. The Petroleum College, Daqing
  • Received:1980-04-21 Online:1981-07-25 Published:2013-07-08

摘要: 对于没有经历过多次构造运动,而且构造运动不很剧烈、地温梯度无太大变化的沉积盆地确定主要生油期,目前国内外一般采用如下方法。(1)对盆地同一生油层系按不同深度进行系统取样、分析,作出该生油层的总烃量或总烃/有机碳比值与深度的关系图,确定该生油层的现在的生油门限深度。根据地温梯度,就可算出现在的生油门限温度。(2)在盆地不同地区的生油层沉降史图上,生油门限深度水平线与生油层沉降线的交点所对应的时间,即为该地区主要生油期的开始时间。

Abstract: In studying the threshold temperature(depth)of oil generation of the source rocks in Qijia-Gulong and Sanzhao depressions in the Songliao Basin with J, Cannan time-temperature formula, a correction factor of 18℃ should be applied to negate the error caused by the geothermal differences between the ancient and recent ages. It has been found that oil generation in the Qijia-Gulong depression started at the time of deposition of Sifangtai formation in late Cretaceous, earlier than that in Sanzhao depression which began at the time of deposition of Mingshui formation in late Cretaceous. This is the reason why oil of Daqing field has its origin from the former, and few oil pools occur in the later.