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川西新场须四段致密砂岩储层微观孔喉与可动流体变化特征

肖开华 冯动军 李秀鹏

肖开华, 冯动军, 李秀鹏. 川西新场须四段致密砂岩储层微观孔喉与可动流体变化特征[J]. 石油实验地质, 2014, 36(1): 77-82. doi: 10.11781/sysydz201401077
引用本文: 肖开华, 冯动军, 李秀鹏. 川西新场须四段致密砂岩储层微观孔喉与可动流体变化特征[J]. 石油实验地质, 2014, 36(1): 77-82. doi: 10.11781/sysydz201401077
Xiao Kaihua, Feng Dongjun, Li Xiupeng. Micro pore and throat characteristics and moveable fluid variation of tight sandstone in 4th member of Xujiahe Formation, Xinchang Gas Field, western Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(1): 77-82. doi: 10.11781/sysydz201401077
Citation: Xiao Kaihua, Feng Dongjun, Li Xiupeng. Micro pore and throat characteristics and moveable fluid variation of tight sandstone in 4th member of Xujiahe Formation, Xinchang Gas Field, western Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(1): 77-82. doi: 10.11781/sysydz201401077

川西新场须四段致密砂岩储层微观孔喉与可动流体变化特征

doi: 10.11781/sysydz201401077
基金项目: 中国石油化工股份有限公司科技项目“新场须四段致密气藏描述(P12109)”资助。
详细信息
    作者简介:

    肖开华(1963-),男,硕士,高级工程师,从事油气地质综合研究。E-mail:xiaokh.syky@sinopec.com。

  • 中图分类号: TE132.2

Micro pore and throat characteristics and moveable fluid variation of tight sandstone in 4th member of Xujiahe Formation, Xinchang Gas Field, western Sichuan Basin

  • 摘要: 为了评价川西新场须四段致密砂岩储层,应用恒速压汞及核磁共振实验方法对储层微观孔喉与可动流体变化特征进行定量分析。结果表明,须四段致密砂岩储层可动流体参数、喉道特征参数及孔隙参数变化幅度大。微裂隙发育的致密砂岩储层孔隙对可动流体参数的影响较喉道要更大一些,在微观上可动流体参数主要受孔隙控制。孔喉半径比较大、分布范围宽是致密砂岩储层可动流体含量低、可动用程度差的主要原因之一。微裂隙发育的致密砂岩储层具有喉道进汞饱和度较孔隙进汞饱和度高的特点,说明新场须四段致密砂岩储层的储集空间类型主要为孔隙—裂缝型。

     

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出版历程
  • 收稿日期:  2013-09-25
  • 修回日期:  2013-11-26
  • 刊出日期:  2014-01-28

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