首页> 外文期刊>Earth sciences research journal >Fractal characteristics of reservoir structural fracture: a case study of Xujiahe Formation in central Yuanba area. Sichuan Basin
【24h】

Fractal characteristics of reservoir structural fracture: a case study of Xujiahe Formation in central Yuanba area. Sichuan Basin

机译:储层构造裂缝的分形特征-以元坝中部地区须家河组为例。四川盆地

获取原文
           

摘要

The reservoir structural fractures have excellent fractal characteristics, as well as self-similarities. Based on the fractal theory, the surface fractal characteristics of faults and the fractal characteristic of fractures in the core of the Xujiahe Formation in the Fault-Fold Belt of the central Yuanba area were studied, and a quantitative relationship was set up between them. Based on the fractal characteristics of faults, predictions were made of the favorable fracture zone, which provides a new idea for the research of fracture, as well as offers theoretical references for exploring the fracture development zone during oil-gas exploration. The results show the following: the seismic value of reflection fault fractal dimension of the Xujiahe Formation is 1.5284; the correlation coefficient R2 is bigger than 0.9901; the capacity dimension linear regression correlation coefficient of the fracture in core of the Xujiahe Formation is bigger than 0.98; the fractal dimension D can well reflect the fault and fracture development degree, as well as the complexity of the fracture system; it can quantitatively calculate the density of the fracture of the reservoir in the area; the areas of capacity dimension bigger than 1.45 are the fracture development zones in the Fault-Fold Belt of the central Yuanba area; the oil and gas enrichment degree is high; the areas with the fractal dimension value between 0.95 and 1.45 are the fracture relatively-developed zones; the fractal dimension with values smaller than 0.95 are the lack of fracture areas.
机译:储层构造裂缝具有极好的分形特征和自相似性。基于分形理论,研究了中部元坝地区褶皱带中断层的表面分形特征和徐家河组岩心的裂缝分形特​​征,并建立了定量关系。根据断层的分形特征,对有利的裂缝带进行了预测,为裂缝的研究提供了新思路,为油气勘探过程中裂缝发育带的勘探提供了理论参考。结果表明:徐家河组反射断层分形维数的地震值为1.5284。相关系数R2大于0.9901;徐家河组岩心裂缝的能力维数线性回归相关系数大于0.98。分形维数D可以很好地反映断层和裂缝的发育程度,以及裂缝系统的复杂性。它可以定量计算该地区储层的裂缝密度。容量尺寸大于1.45的区域是元坝中部断层褶皱带的裂缝发育带;油气富集度高。分形维数在0.95-1.45之间的区域是裂缝相对发育的区域。小于0.95的分形维数是缺少断裂区域。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号