松辽盆地朝长地区未熟、低熟烃源岩排烃研究

郝黎明; 郝石生

doi:10.11781/sysydz200001064

松辽盆地朝长地区未熟、低熟烃源岩排烃研究

doi: 10.11781/sysydz200001064

郝黎明¹,
郝石生²

1.
中国矿业大学北京校区, 北京 100083
2. 石油大学(北京)地科系, 北京 100083

基金项目: 中国石油天然气集团公司"九·五"重点科技攻关项目《中国未熟-低熟石油的成因机制、成藏条件和资源预测》(960006)的部分成果

详细信息

作者简介:
郝黎明(1973- ),男,甘肃酒泉人,博士生,主要研究方向为沉积学与层序地层学.

中图分类号: TE135.2
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- 被引次数: 0
出版历程
- 收稿日期: 1998-10-30
- 修回日期: 1999-11-25
- 刊出日期: 2000-01-25

HYDROCARBON EXPULSION OF IMMATURE AND LOW-MATURE SOURCE ROCKS IN CHAOCHANG AREA OF THE SONGLIAO BASIN

HAO Li-ming¹,
HAO Shi-sheng²

1.
China University of Mining and Technology, Beijing 100083, China
2. University of Petroleum, Beijing 100083, China

摘要

摘要: 本文利用实验室模拟方法研究了松辽盆地朝(朝阳沟)长(长春岭)地区白垩系和外围汤元地区第三系低熟源岩的排烃过程,样品分别在150℃、200℃、250℃、300℃4个温度点各作一次实验。结果表明,低熟源岩的排烃过程具有“地质色层效应”,主要表现在排出烃与残留烃的族组成、气相色谱以及生物标志化合物等指标的差异上。本文计算并校正了模拟实验各温度点的排烃量和排烃效率,得出了朝长地区低熟源岩排烃效率与演化程度的经验公式。研究认为,低熟源岩排烃主要受源岩有机质丰度、类型、热演化成熟度及地下水活动等因素的影响。本区低熟源岩具有良好的生烃能力和排烃潜力,故具有良好的油气资源前景。
- 排烃量 /
- 排烃效率 /
- 低熟源岩 /
- 白垩系 /
- 朝长地区
Abstract: In this paper,the hydrocarbon expulsion course of low mature source rocks from the Cretaceous of Chaochang area and the Tertiary of peripheral Tangyuan area in the Songliao Basin is studied by laboratory simulation.We experiment upon samples at 150℃,200℃,250℃ and 300℃,respectively.The results suggest that the geo chromatographic effects do exist during the hydrocarbon expulsion course of low mature source rocks,which are shown mainly by the differences of group composition,gas chromatogram and biomarkers between expelled and residual hydrocarbon.We also figure and correct the hydrocarbon expulsion quantity and efficiency in the simulation experiment at each temperature point,and obtain the experience formulation for the hydrocarbon expulsion efficiency and evolutionary degree of low mature source rocks in Chaochang area.It is considered that the hydrocarbon expulsion of low mature source rocks is mainly controlled by the abundance,types and thermal evolutionary maturity of organic matter and the movement of groundwater.The low mature source rocks of this area have good hydrocarbon generation capability and hydrocarbon expulsion potential,so they have good prospects for hydrocarbon resources.
- hydrocarbon-expulsion quantity /
- hydrocarbon expulsion efficiency /
- low mature source rocks /
- the Cretaceous /
- Chaochang area

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参考文献(9)

[1]	王铁冠,钟宁宁,等,低熟油气形成机理与分布[M].北京:石油上业出版社,1995.
[2]	中国石油地质志编委会编.中国石油地质志(卷二,上)—大庆油田[M].北京:石油工业出版社,1993.
[3]	郝石生,陈章明,等.吐哈盆地台北凹陷煤系地层油气运移及资源评价[M].北京中油科技开发公司,1995.
[4]	藏卿林,郝石生,等.煤与泥岩排烃过程中甾、萜烷色层效应差异[J].地球化学,1996,25(4).
[5]	侯读杰,王铁冠,等.陆相油气地球化学研究.武汉:中国地质大学出版社,1995.
[6]	E Lafergue,J Espitalie.Experimental simulation of primary migration[J].Organic Geochemistry,1994,22(3～5):575～586.
[7]	Peters,Moldowan.生物标记化合物指南[M].姜乃煌,张水昌,等译.北京:石油工业出版社,1995.
[8]	冯子辉,等.松辽及外围盆地未熟、低熟油研究中期汇报资料[R].内部资料,1997.
[9]	W K Seifert,J M Moldowan.Paleoreconstruction by biological markers [J].Geochim Cosmochim Acta,1981,45:783～794.