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准噶尔盆地春晖油田石炭系火山岩储层控制因素分析

董臣强

董臣强. 准噶尔盆地春晖油田石炭系火山岩储层控制因素分析[J]. 沉积与特提斯地质, 2014, 34(2): 92-97.
引用本文: 董臣强. 准噶尔盆地春晖油田石炭系火山岩储层控制因素分析[J]. 沉积与特提斯地质, 2014, 34(2): 92-97.
DONG Chen-qiang. Controlling factors of the Carboniferous volcanic reservoirs in the Chunhui Oil Field, Junggar Basin[J]. Sedimentary Geology and Tethyan Geology, 2014, 34(2): 92-97.
Citation: DONG Chen-qiang. Controlling factors of the Carboniferous volcanic reservoirs in the Chunhui Oil Field, Junggar Basin[J]. Sedimentary Geology and Tethyan Geology, 2014, 34(2): 92-97.

准噶尔盆地春晖油田石炭系火山岩储层控制因素分析

基金项目: 

国家科技重大专项“准噶尔盆地碎屑岩层系大中型油气田形成规律与勘探方向”(2011ZX05002-002)

国家重点基础研究发展计划(973)项目“中国西部典型叠合盆地油气成藏机制与分布规律”

中国石油化工股份有限公司重大科技攻关项目“准西北地区超剥带成藏规律及勘探目标”(P12028)

详细信息
    作者简介:

    董臣强(1970-),男,博士,高级工程师。E-mail:dcq010@163.com

  • 中图分类号: TE122.2+22

Controlling factors of the Carboniferous volcanic reservoirs in the Chunhui Oil Field, Junggar Basin

  • 摘要: 春晖油田石炭系火山岩地层中,油气富集程度与储层发育程度呈正相关关系。研究认为,储层的发育与分布主要受岩相、岩性和构造运动的控制。岩相控制岩性,岩性控制储集空间组合类型,溢流相和火山沉积相围绕爆发相具有环带状分布特点,从火山角砾岩→玄武岩、安山岩→凝灰岩,储集性能逐渐变差;构造运动则控制裂缝的发育及溶蚀作用,断层周边微裂缝发育,沿着微裂缝则溶蚀作用增强,次生孔隙发育。
    Abstract: The Chunhui Oil Field in the Junggar Basin lies in the western part of the Halaalate Mountain tectonic zone, in which the Carboniferous volcanic strata consist dominantly of the volcanic rocks such as tuff, andesite, basalt and volcanic breccias. There is a positive correlation between the hydrocarbon enrichment and reservoir development in the Carboniferous volcanic reservoir rocks from the Chunhui Oil Field. The distribution and development of the volcanic reservoir rocks are primarily controlled by lithofacies, lithology and tectonism. On the whole, the lithofacies may exercise a major control on lithology of the volcanic reservoir rocks, which, in turn, may control the reservoir spaces types. The volcanic rocks in the Chunhui Oil Field exhibit a trend of the girdle pattern of lithofacies changes from the explosive facies through the effusive facies to the volcano-sedimentary facies. The reservoir capacity is gradually getting poor and poor from volcanic breccias to basalt and andesite and finally to tuff. The tectonism is also believed to be a major control on the fissure development and dissolution. The structural stress may give rise to the formation of the cracks or fissures in the brittle rocks, which may greatly improve the reservoir spaces of the Carboniferous volcanic reservoir rocks in the study area.
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出版历程
  • 收稿日期:  2013-10-23
  • 修回日期:  2013-11-05
  • 发布日期:  2014-06-29

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