岩性油气藏 ›› 2020, Vol. 32 ›› Issue (3): 104–114.doi: 10.12108/yxyqc.20200310

• 油气地质 • 上一篇    下一篇

二连盆地呼仁布其凹陷南洼下白垩统烃源岩分布特征与油源分析

山鑫杰1,2, 王飞宇1,2, 刘念1,2, 冯伟平1,2, 江涛1,2, 杜喜1,2, 程志强1,2, 李思嘉1,2, 李月1,2   

  1. 1. 中国石油大学(北京)地球科学学院, 北京 102249;
    2. 中国石油大学(北京)油气资源与探测国家重点实验室, 北京 102249
  • 收稿日期:2019-09-16 修回日期:2019-10-17 出版日期:2020-05-21 发布日期:2020-04-30
  • 第一作者:山鑫杰(1994-),女,中国石油大学(北京)在读硕士研究生,研究方向为油气地球化学。地址:(102249)北京市昌平区府学路18号。Email:shxinjie@163.com。
  • 基金资助:
    国家科技重大专项“中国典型盆地气源灶和大中型气田形成”（编号：2016ZX05007001-003）与中国石油华北油田科技项目“二连盆地烃源灶与油气成藏”（编号：HBYT-YJY-2017-JS-152）联合资助

Distribution characteristics and oil-source analysis of Lower Cretaceous source rock in southern trough of Hurenbuqi sag，Erlian Basin

SHAN Xinjie1,2, WANG Feiyu1,2, LIU Nian1,2, FENG Weiping1,2, JIANG Tao1,2, DU Xi1,2, CHENG Zhiqiang1,2, LI Sijia1,2, LI Yue1,2   

  1. 1. College of Geosciences, China University of Petroleum(Beijing), Beijing 102249, China;
    2. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum(Beijing), Beijing 102249, China
  • Received:2019-09-16 Revised:2019-10-17 Online:2020-05-21 Published:2020-04-30

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摘要： 呼仁布其凹陷位于二连盆地西部的巴音宝力格隆起中段，前期勘探已发现优质烃源岩和较好的油气显示，但凹陷南洼烃源岩的研究还比较薄弱。通过对呼仁布其凹陷南洼烃源岩测井地球化学评价以及烃源岩和原油样品的有机地球化学对比，揭示了其下白垩统烃源岩有机相分布、烃源岩地球化学特征和油源关系。结果表明：呼仁布其凹陷南洼下白垩统烃源岩主要分布于南洼漕东部，发育阿尔善组、腾一段和腾二段等3套烃源岩，其中阿尔善组烃源岩处于低成熟—成熟阶段，腾一段烃源岩处于低成熟阶段，腾二段烃源岩处于未成熟—低成熟阶段。呼仁布其凹陷南洼下白垩统3个层段均发育C相和D/E相烃源岩，其中，C相烃源岩主要分布于腾一段，厚度为300～400 m，初始氢指数为400～800 mg（/g TOC），显微组分多为腐泥组、壳质组和镜质组，母质来源主要为藻类等低等水生生物，形成于微咸水—半咸水、还原环境；D/E相烃源岩主要分布于阿尔善组，厚度为100～200 m，初始氢指数为200～400 mg（/g TOC），显微组分多为壳质组、镜质组和惰质组，母质来源主要为陆源高等植物，形成于淡水—微咸水、弱还原环境。油源对比认为：阿尔善组的成熟原油来源于阿尔善组烃源岩，腾一段成熟度较低的原油来源于腾一段烃源岩，而腾二段的原油可能来源于腾一段烃源岩。

关键词: 有机相, 油源分析, 阿尔善组, 腾格尔组, 下白垩统, 二连盆地

Abstract: The Hurenbuqi sag is located in the middle of the Bayinbaolige uplift in the western part of the Erlian Basin. It is one of the many oil-rich sags in the Erlian Basin. The early exploration has found high-quality source rocks and better oil and gas display,but the current research on source rock is weak. The study of source rocks is still relatively weak. Based on the geochemical evaluation of source rock and the organic geochemical analysis of source rock and crude oil samples,the distribution of organic facies and geochemical characteristics of source rocks and oil-source relationships in the southern trough of the Huerenbuqi sag were revealed. The results show that the source rocks of the southern trough in the Huerenbuqi sag are mainly distributed in the eastern belt,and three sets of source rocks in the K1 ba,K1 bt1 and K1 bt2 are developed. The source rocks of the K1 ba are in the stage of low maturation,the source rocks of the K1 bt1 are in a low maturation stage,and the source rocks of the K 1 bt2 are in the immature to lowmature stage. The C source rocks and D/E source rocks are developed in the three layers of the Lower Cretaceous in the southern part of the Hurenbuqi sag. The C source rocks of the main body of the depression are mainly distributed in the K1 bt1,the thickness is 300-400 m,the initial hydrogen index is 400- 800 mg/g TOC,and the maceral is composed of sapropelinite and exinite and vitrinite. The parent material is mainly low level aquatic organisms such as algae,formed in brackish water to salt water and reducing environment. The D/E source rocks are mainly distributed in the K1 ba,with a thickness of 100-200 m,the initial hydrogen index is 200-400 mg/g TOC,and the microscopic composition is mainly composed of exinite,vitrinite and inertinite. The parent material is mainly terrestrial plants formed in fresh water to micro-salt water and weak reducing environment. The hydrocarbon center is located in the eastern belt. According to the oil-source analysis,the mature crude oil of the K1 ba was derived from the source rocks of the K1 ba. The low mature crude oil of the K1 bt1 was derived from the source rocks of the K1 bt1,while the crude oil of the K1 bt2 may be derived from the K1 bt1 source rock.

Key words: organic facies, oil source analysis, Alshan Formation, Tenger Formation, Lower Cretaceous, Erlian Basin

中图分类号: 

  • TE122.1+13
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