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川西孝泉—新场地区须家河组四段裂缝分布特征

张克银

张克银. 川西孝泉—新场地区须家河组四段裂缝分布特征[J]. 石油实验地质, 2014, 36(4): 398-404. doi: 10.11781/sysydz201404398
引用本文: 张克银. 川西孝泉—新场地区须家河组四段裂缝分布特征[J]. 石油实验地质, 2014, 36(4): 398-404. doi: 10.11781/sysydz201404398
Zhang Keyin. Fracture distribution characteristics of 4th member of Xujiahe Formation in Xiaoquan-Xinchang area, western Sichuan[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(4): 398-404. doi: 10.11781/sysydz201404398
Citation: Zhang Keyin. Fracture distribution characteristics of 4th member of Xujiahe Formation in Xiaoquan-Xinchang area, western Sichuan[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(4): 398-404. doi: 10.11781/sysydz201404398

川西孝泉—新场地区须家河组四段裂缝分布特征

doi: 10.11781/sysydz201404398
基金项目: 国家科技重大专项课题“四川盆地碎屑岩层系大中型油气田形成规律与勘探方向”(2011ZX05002-004)资助。
详细信息
    作者简介:

    张克银(1967—),男,高级工程师,从事油气地质综合研究。E-mail: zhang_ky99@126.com。

  • 中图分类号: TE122.2+3

Fracture distribution characteristics of 4th member of Xujiahe Formation in Xiaoquan-Xinchang area, western Sichuan

  • 摘要: 通过电成像测井的手段,对研究区内19口重点井须家河组四段发育的天然裂缝资料进行了统计、分析,认为该层位裂缝主要有4组:印支晚期—燕山早期的NE-SW向裂缝,燕山中、晚期的近SN向裂缝,喜马拉雅晚期的NW-SE向裂缝和喜马拉雅期四幕的ESE-WNW至ENE-WSW向裂缝;孝泉—新场地区须家河组四段主要发育低角度斜交裂缝以及高角度斜交裂缝,水平缝发育较少,垂直缝基本不发育;背斜南、北两翼的裂缝线密度要大于轴部,背斜轴部总体上表现为距断裂系统越近、裂缝的线密度越大的特点;裂缝线密度的不均质性较强;中砂岩、细砂岩、砾岩、粗砂岩是裂缝的主要载体,裂缝在中砂岩、细砂岩、砾岩、粗砂岩中发育得更好,而页岩中的裂缝最不发育;页岩、泥质粉砂岩、粉砂岩中的裂缝线密度呈较清晰的随层厚增加而减小的趋势;粉砂质页岩、粗砂岩中裂缝线密度与层厚没有表现出明显的对应关系。

     

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出版历程
  • 收稿日期:  2014-01-10
  • 修回日期:  2014-06-10
  • 刊出日期:  2014-07-28

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