西南石油大学学报(自然科学版) ›› 2007, Vol. 29 ›› Issue (3): 28-31.DOI: 10.3863/j.issn.1000-2634.2007.03.008

• 地质勘探 • 上一篇    下一篇

陇东西峰地区延长组烃源岩热演化程度研究

吉利明 1,2 李林涛 1,3 吴 涛 1,3

  

  1. (1.中国科学院地质与地球物理研究所 兰州油气资源研究中心 气体地球化学重点实验室,甘肃 兰州 730000;2.中国地质大学研究生院,湖北 武汉 430074;3.中国科学院研究生院,北京 100069)
  • 收稿日期:2006-04-10 修回日期:1900-01-01 出版日期:2007-06-20 发布日期:2007-06-20
  • 通讯作者: 吉利明

THERMAL EVOLUTION OF SOURCE ROCKS INYANCHANG FORMATION, XIFENG AREA,EAST GANSU PROVINCE

JI Li-ming 1,2,LI Lin-tao 1,3,WU Tao 1,3

  

  1. (Research Center for Oil and Gas Resource,Institute of Geology and Geophysics,Chinese Academy of Science,Lanzhou Gansu 730000,China)
  • Received:2006-04-10 Revised:1900-01-01 Online:2007-06-20 Published:2007-06-20
  • Contact: JI Li-ming

摘要: 利用热分析、可溶有机质分析、干酪根镜质体反射率及生物标志物参数等,对与油藏有密切关系的延长组长8—长7段进行了热成熟度研究。烃源岩热解峰温、沥青和烃转化率、Ro值、OEP值、C29 ααα-20S/(20S+20R)甾烷参数值和C31 αβ-22S/(22S+22R)藿烷参数值均指示,长8—长7段烃源岩整体处于大量生烃的成熟有机质演化阶段,并已达到生油高峰,具备有利的生排烃条件。尽管西峰地区不同井位的构造位置和现今地层埋深各不相同,但经历了相近的沉降与热演化历史,长8—长7段烃源岩具有一致的热演化程度。为全面揭示鄂尔多斯盆地西南部西峰地区延长组烃源岩的生、排烃能力,提供了基础资料。

关键词: 延长组, 烃源岩, 热成熟度, 西峰油田, 鄂尔多斯盆地

Abstract: In order to comprehensively reveal the hydrocarbon generation and expulsion ability of source rocks of the Yanchang Formation in Xifeng area, Southwestern Ordos Basin, the authors investigates the maturity degree of source rocks in the Member 8 and 7 of Yanchang Formation which are closely related to the reservoir. pyrolysis analysis, dissolvable organic matter analysis, vitrinite reflectance of kerogen and biomarker parameter are applied in the research. The peak temperatures of Rock-Eval pyrolysis, conversion rates of bitumen and hydrocarbon, Ro values, OEP values, sterane parameter C29ααα-20S/(20S+20R) and hopane parameter C31αβ-22S/(22S+22R) all indicate that the source rocks in Member 8 and 7 are in the mature stage of organic matter and have reached the peak of hydrocarbon generation. Therefore the source rocks have provided with advantageous conditions to generating and expulsion of hydrocarbon. Although the structure position and buried depth of strata of different wells in Xifeng area are difference at present, the source rocks in Member 8 and 7 of Yanchang Formation have identical thermal evolution because of the similar subsidence history and thermal history. The study provides the basic information for wholly revealing the generating and expulsing ability of the source rocks in the formation.

Key words: Yanchang formation, source rock, thermal maturity degree, Xifeng oil field, Ordos basin 

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