首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >From fractures to flow: A field-based quantitative analysis of an outcropping carbonate reservoir
【24h】

From fractures to flow: A field-based quantitative analysis of an outcropping carbonate reservoir

机译:从裂缝到流动:露头碳酸盐岩储层的基于现场的定量分析

获取原文
获取原文并翻译 | 示例
           

摘要

Fractures can play an important role in the fluid storage-migration properties of fault damage zones. In this present contribution, we document the role exerted by fractures on fluid flow in carbonate damage zones of hydrocarbon-bearing, km-long, oblique-slip normal faults with 10's of m-throw. The carbonate fault damage zones were analysed by mean of scan line surveys conducted in both tar-free and tar-rich outcrops. In this way, the relationships among the individual fracture characteristics (length, spacing, aperture, orientation, connectivity and distance from slip surfaces pertaining to small faults of the fault damage zones) and hydrocarbons have been established. Data obtained by scan line surveys were also used to compute the amount of fracture porosity, the degree of fracture connectivity and, based upon simple assumptions, the orientation of the local σ_(hmax) at times of faulting. Additionally, scan line surveys were also carried out along outcrops exposing unfaulted carbonate host rocks. The results of our computation are consistent with a carbonate host rock made up of a quite isotropic fracture array comprised of isolated and coupled fractures, in which individual fracture sets have negative exponential spacing distributions. In terms of fluid flow, the fracture array of the carbonate host rock enhances the fluid storage. Conversely, the fracture array of the fault damage zones is characterized by a pronounced anisotropy due to interconnected fractures, which enhance the fluid migration. Fractures in the fault damage zones include those inherited from background deformation and others related to the faulting processes. The latter fracture sets are characterized by power law spacing distributions. In conclusion, counter-intuitively, both fracture length and fracture spacing do not have any correlation with hydrocarbons in the fault damage zones. On the contrary, fracture anisotropy, fracture spread and fracture orientation are positively correlated with hydrocarbons.
机译:断裂在断层破坏带的流体运移运移特性中起着重要作用。在目前的贡献中,我们记录了裂缝对含碳氢化合物,千米长,斜滑正断层的碳酸盐岩破坏带中的流体的作用,该断层的m倾角为10s。通过在不含焦油和富含焦油的露头进行的扫描线调查分析了碳酸盐岩断层破坏带。以这种方式,已经建立了各个断裂特征(长度,间距,孔径,取向,连通性和与滑动面的距离,该滑动面与断裂破坏带的小断裂有关)与烃之间的关系。通过扫描线勘测获得的数据还用于计算裂缝孔隙度,裂缝连通度,并基于简单的假设计算出断层时局部σ_(hmax)的方向。另外,还沿着露头进行了扫描线调查,露出未断裂的碳酸盐岩。我们的计算结果与碳酸盐岩基质岩石一致,碳酸盐岩基质由相当各向同性的裂缝阵列组成,这些裂缝阵列由孤立的和耦合的裂缝组成,其中各个裂缝组具有负指数间距分布。在流体流动方面,碳酸盐岩的裂隙排列增加了流体的储存。相反,断层破坏带的裂缝阵列的特征是由于相互连接的裂缝而引起的明显的各向异性,从而增加了流体的运移。断层破坏带中的裂缝包括从背景变形中继承的裂缝以及与断层过程有关的其他裂缝。后一组裂缝的特征在于幂律间距分布。总之,与直觉相反,断裂长度和断裂间距与断层破坏带中的碳氢化合物没有任何关系。相反,裂缝的各向异性,裂缝的扩展和裂缝的方向与碳氢化合物呈正相关。

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