石油与天然气地质 ›› 1981, Vol. 2 ›› Issue (4): 359-368.doi: 10.11743/ogg19810408

• 论文 • 上一篇    下一篇

塔里木盆地石油有机地球化学特征和油源问题探讨

胡伯良   

  1. 中国科学院兰州地质研究所
  • 出版日期:1981-12-25 发布日期:2012-01-16

ON THE ORGANIC GEOCHEMICAL CHARACTERISTICS AND OIL-SOURCE CORRELATIONS IN TARIM BASIN

Hu Boliang   

  1. Lanzhou Geological Institute, Academia Sinica
  • Online:1981-12-25 Published:2012-01-16

摘要:

油源岩的有机地球化学特征塔里木盆地有巨厚的沉积盖层,其中主要的生油岩系有三套。一 三套油源岩的沉积特征和有机质丰度1.石炭—二叠系 石炭系以海相碳酸盐岩为主,在中、下石炭统夹有厚层的碳质页岩和石英砂岩。碳酸盐岩中含有丰富的珊瑚和腕足类等化石。

Abstract:

In this paper,by using of some advanced techniques,the organic geoche-mical characteristics of the crude oil and its possible source rocks in Tarimbasin and their oil-source correlations have been studied and presented here.It is pointed out that,in Tarim,the marine beds of Upper Cretaceous-Low-er Tertiary is a moderate source rock only;the Jurassic lacustrine formationis rich in organic matter and may be the best source bed in this basin,but itis distributed only in some local areas,such as Kuqa and Kashi depressions;the Permo-Carboniferous system has a relatively low content of organic mat-ter,but it is widespread and very thick,therefore,it may be the most poten-tial source bed for oil and gas among the three possible source beds in the basin.The high-yield crude oil and gas in the continental Miocene of the Keke-ya oil field are highly maturated and characterized by terrigenous origin,therefore,the author believes that they may migrate from Permo-Carboni-ferous source beds.Some crude oil in the Kuqa depression is marked by marine origin,whichshows that the Meso-Cenozaic in this area may contain some marine sourcebeds.