In this study we present a step-by-step theoretical modelling approach, using established seismic wave propagation theories in anisotropic media, to generat'/> Modelling Orthorhombic Anisotropic Effects for Reservoir Fracture Characterization of a Naturally Fractured Tight Carbonate Reservoir, Onshore Texas, USA
首页> 外文期刊>Pure and Applied Geophysics >Modelling Orthorhombic Anisotropic Effects for Reservoir Fracture Characterization of a Naturally Fractured Tight Carbonate Reservoir, Onshore Texas, USA
【24h】

Modelling Orthorhombic Anisotropic Effects for Reservoir Fracture Characterization of a Naturally Fractured Tight Carbonate Reservoir, Onshore Texas, USA

机译:建模正交骨质骨折岩浆骨折特征天然骨折碳酸盐岩储层,美国陆上德克萨斯州

获取原文
获取原文并翻译 | 示例
           

摘要

AbstractIn this study we present a step-by-step theoretical modelling approach, using established seismic wave propagation theories in anisotropic media, to generate unique anisotropic reflection patterns observed from three-dimensional pure-mode pressure (3D-PP), full-azimuth and full-offset seismic reflection data acquired over a naturally fractured tight carbonate field, onshore Texas, USA. Our aim is to gain an insight into the internal structures of the carbonate reservoir responsible for the observed anisotropic reflection patterns. From the generated model we were able to establish that the observed field seismic reflection patterns indicate azimuthal anisotropy in the form of crack induced shear-wave splitting and variation in P-wave velocity with offset and azimuth. Amplitude variation with azimuth (AVAZ) analysis also confirmed multi-crack sets induced anisotropy which is characteristic of orthorhombic symmetry, evident as multiple bright and dim-amplitude azimuth directions as well as complete reversal of bright-amplitude to dim-amplitude azimuth direction as the angle of incidence increases from near (≤15°) to mid (≥30°) offsets. Finally, we fitted the generated P-wave velocity into an?ellipse to determine the intensity and orientation (N26E) of the open crack set as well as the direction of the minimum in situ stress axis (N116E) within the reservoir. The derived information served as an?aid for the design of horizontal well paths that would intercept open fractures and ensure production optimization of the carbonate reservoir, which was on production decline despite reservoir studies that indicate un-depleted reserves.
机译:Abstract在本研究中,我们提出了一种逐步的理论建模方法,使用各向异性介质中已建立的地震波传播理论,生成从三维纯模式压力(3D-PP)观察到的独特各向异性反射模式,全方位和全偏移距地震反射数据采集自美国德克萨斯州陆上的天然裂缝致密碳酸盐岩油田。我们的目标是深入了解碳酸盐岩储层的内部结构,这些结构与观测到的各向异性反射模式有关。根据生成的模型,我们能够确定,观测到的现场地震反射模式表明方位各向异性,表现为裂缝引起的剪切波分裂以及P波速度随偏移距和方位角的变化。振幅随方位角变化(AVAZ)分析也证实了多裂纹组诱发的各向异性,这是正交对称的特征,明显表现为多个明暗振幅方位角方向,以及随着入射角从近距离增加,明暗振幅方位角方向完全反转(≤15°)到中间(≥30°)偏移。最后,我们将生成的P波速度拟合为?椭圆,以确定裂缝组的强度和方向(N26E)以及储层内最小地应力轴(N116E)的方向。导出的信息作为一个?帮助设计水平井路径,拦截开放裂缝,确保碳酸盐岩储层的产量优化,尽管储层研究表明未枯竭储量,但碳酸盐岩储层的产量仍在下降

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