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Determination of seismic anisotropy parameters from multicomponent vertical seismic profiles for improved seismic imaging and reservoir characterization.

机译:从多分量垂直地震剖面中确定地震各向异性参数,以改善地震成像和储层特征。

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摘要

Multicomponent vertical seismic profile (VSP) data can be used to determine seismic anisotropy more accurately. First, I modify the slowness-polarization method by including both P- and SV-wave data for estimating the anisotropy parameters delta and eta of VTI (transversely isotropic with vertical symmetry axis) media. Then I apply the technique to a multicomponent VSP dataset from the Wattenberg Field in Colorado, USA.;The importance of the derived anisotropic velocity model from the joint P- and SV- wave slowness-polarization method for reservoir characterization at the Wells Ranch VSP area is: 1) identifying the possible existence of open fracture networks in the Niobrara Formation at the VSP well location, 2) improving the quality of the Niobrara Formation image which is vital for future drilling programs, 3) accurately depicting the structure in the well vicinity and finally 4) determining elastic properties of the Niobrara reservoir. To identify the existence of open fracture networks, azimuthal AVO response of top of the Niobrara Formation at the VSP well is analyzed. To correct the azimuthal AVO response for propagation phenomena, using the anisotropic velocity model from the joint slowness- polarization method, I modified the moveout-based anisotropic spreading correction (MASC) technique for the VSP data.;The azimuthal AVO analysis shows very weak azimuthal anisotropy at the top of Niobrara Formation near the VSP well. This result indicates the lack of open natural fractures at the Niobrara Formation in this area and explains the low production associated with the well. In addition, I used the anisotropic velocity model obtained from the joint slowness-polarization method to build a 2D VSP image. Comparing the final VSP images using the isotropic and anisotropic velocity models with well data shows that the anisotropic image is more accurately depicted and if inverted would give more robust elastic parameter definition.
机译:多分量垂直地震剖面(VSP)数据可用于更准确地确定地震各向异性。首先,我通过同时包含P波和SV波数据来修改慢度极化方法,以估计VTI(垂直对称轴的横观各向同性)介质的各向异性参数δ和eta。然后将该技术应用于美国科罗拉多州Wattenberg油田的多组分VSP数据集;;从P波和SV波联合慢度极化方法导出的各向异性速度模型对于Wells Ranch VSP地区的储层表征的重要性是:1)确定VSP井位Niobrara地层中可能存在裸眼裂缝网络; 2)改善Niobrara地层图像的质量,这对于未来的钻井计划至关重要; 3)准确描绘井附近的结构最后4)确定Niobrara储层的弹性。为了确定开放裂缝网络的存在,分析了VSP井Niobrara组顶部的方位AVO响应。为了校正传播现象的方位AVO响应,我使用了联合慢度-极化方法中的各向异性速度模型,对VSP数据修改了基于偏移的各向异性扩展校正(MASC)技术。方位AVO分析表明,方位角非常弱VSP井附近Niobrara组顶部的各向异性。该结果表明该地区Niobrara组缺乏裸露的天然裂缝,并解释了与该井相关的低产。此外,我使用了从联合慢极化方法获得的各向异性速度模型来构建2D VSP图像。使用各向同性和各向异性速度模型将最终的VSP图像与油井数据进行比较,结果表明,各向异性图像的描绘更为准确,如果反转,则弹性参数定义也更加可靠。

著录项

  • 作者

    Tamimi, Naser.;

  • 作者单位

    Colorado School of Mines.;

  • 授予单位 Colorado School of Mines.;
  • 学科 Geophysics.
  • 学位 Ph.D.
  • 年度 2015
  • 页码 122 p.
  • 总页数 122
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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