天然气地质学

准噶尔盆地陆西地区石炭系火山岩储层发育主控因素分析

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  • 1.中国科学院油气资源研究重点实验室,甘肃 兰州 730000;
    2.中国科学院资源环境科学信息中心/中国科学院国家科学图书馆兰州分馆,甘肃 兰州 730000;
    3.中国科学院研究生院,北京 100049
李小燕(1982-),甘肃静宁人,助理编辑,硕士,主要从事油气储层地质研究及科技期刊编辑工作.

收稿日期: 2010-02-06

  修回日期: 2010-04-18

  网络出版日期: 2010-06-10

基金资助

国家油气重大专项项目(编号:2008ZX05008-003-04)资助.

Principal Controls on the Formation of Volcanic  Reservoir (Carboniferous) in Luxi Area of Junggar Basin

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  • 1. Key Laboratory of Petroleum Resources Research, Institute of Geology and Geophysics,ChineseAcademy of Sciences, Lanzhou 730000,China;2. Scientific Information Center for Resources and Environment /Lanzhou Branch of National Science Library, Chinese Academy of Sciences,Lanzhou 730000,China;
    3. Graduate University of Chinese Academy of Sciences, Beijing 100049,China

Received date: 2010-02-06

  Revised date: 2010-04-18

  Online published: 2010-06-10

摘要

通过对岩心和普通薄片的观察、荧光薄片及扫描电镜的分析,从火山岩岩性、孔隙类型、含油气性及成岩作用等方面研究,发现准噶尔盆地陆西地区石炭系火山岩岩性主要以火山熔岩及火山碎屑岩为主。火山熔岩主要包括玄武岩和安山岩,含油气性相对较好。
火山碎屑岩主要为凝灰岩和火山角砾岩.孔隙类型主要以溶蚀孔隙和次生裂缝为主.因火山岩只有经过后期风化淋滤作用、断裂改造作用及溶蚀作用改造后才能成为有效储层,浊沸石充填对研究区优质储层的形成可能具有极好的控制作用。在研究区不同类型火山岩储层的孔隙演化模式。

本文引用格式

李小燕, 王琪, 史基安, 马晓峰, 郝乐伟, 张瑞, 王欢 . 准噶尔盆地陆西地区石炭系火山岩储层发育主控因素分析[J]. 天然气地球科学, 2010 , 21(3) : 449 -457 . DOI: 10.11764/j.issn.1672-1926.2010.03.449

Abstract

By the observation of core and analysis of microscopic flakes and scanning electron microscope, the feature of the Carboniferous volcanic rocks in the Luxi district of Junggar basin was discussed, including volcanic lithology, pore type, oil and gas evidence, and diagenesis. The lithology of main volcanic reservoir in the study area is dominated by volcanic lava (basalt and andesite) and pyroclastic rocks (tuff and volcanic breccia). The pore type is dissolution pore and the secondary dissolution. The volcanic lava has a good oil and gas evidence.The volcanic  reservoir become a good stored body only after weathering and leaching, fracture and dissolved reformation later. The laumontite filling in the study area would make a positive role of the formation of high quality reservoir. Finally, the pattern of porosity evolution for different types of volcanic rocks was setup.

参考文献

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