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Analysis of seismic anisotropy in 3D multi-component seismic data

机译:3D多分量地震数据中的地震各向异性分析

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摘要

The importance of seismic anisotropy has been recognized by the oil industry since itsudfirst observation in hydrocarbon reservoirs in 1986, and the application of seismicudanisotropy to solve geophysical problems has been keenly pursued since then. However,uda lot of problems remain, which have limited the applications of the technology.udNowadays, more and more 3D multi-component seismic data with wide-azimuth areudbecoming available. These have provided more opportunities for the study of seismicudanisotropy. My thesis has focused on the study of using seismic anisotropy in 3Dudmulti-component seismic data to characterize subsurface fractures, improve convertedudwave imaging and detect fluid content in fractured reservoirs, all of which are importantudfor fractured reservoir exploration and monitoring.udFor the use of seismic anisotropy to characterize subsurface fracture systems, equivalentudmedium theories have established the link between seismic anisotropy and fractureudproperties. The numerical modelling in the thesis reveals that the amplitudes and intervaludtravel-time of the radial component of PS converted waves can be used to derive fractureudproperties through elliptical fitting similar to P-waves. However, sufficient offsetudcoverage is required for either the P- or PS-wave to reveal the features of ellipticaludvariation with azimuth.udCompared with numerical modelling, seismic physical modelling provides additionaludinsights into the azimuthal variation of P and PS-wave attributes and their links withudfracture properties. Analysis of the seismic physical model data in the thesis shows thatudthe ratio of the offset to the depth of a target layer (offset-depth ratio), is a key parameterudcontrolling the choice of suitable attributes and methods for fracture analysis. Data withuda small offset-depth ratio from 0.7 to 1.0 may be more suitable for amplitude analysis;udwhilst the use of travel time or velocity analysis requires a large offset-depth ratio aboveud1.0, which can help in reducing the effect of the acquisition footprint and structuraludimprint on the results. Multi-component seismic data is often heavily contaminated with noise, which will limitudits application potential in seismic anisotropy analysis. A new method to reduce noise inud3D multi-component seismic data has been developed and has proved to be very helpfuludin improving data quality. The method can automatically recognize and eliminate strongudnoise in 3D converted wave seismic data with little interference to useful reflectionudsignals.udComponent rotation is normally a routine procedure in 3D multi-component seismicudanalysis. However, this study shows that incorrect rotations may occur for certainudacquisition geometry and can lead to errors in shear-wave splitting analysis. A qualityudcontrol method has been developed to ensure this procedure is correctly carried out.udThe presence of seismic anisotropy can affect the quality of seismic imaging, but theudstudy has shown that the magnitude of the effects depends on the data type and targetuddepth. The effects of VTI anisotropy (transverse isotropy with a vertical symmetry axis)udon P-wave images are much weaker than those on PS-wave images. Anisotropic effectsuddecrease with depth for the P- and PS-waves. The real data example shows that theudoverall image quality of PS-waves processed by pre-stack time migration has beenudimproved when VTI anisotropy has been taken into account. The improvements areudmainly in the upper part of the section.udMonitoring fluid distribution is an important task in producing reservoirs. A syntheticudstudy based on a multi-scale rock-physics model shows that it is possible to use seismicudanisotropy to derive viscosity information in a HTI medium (transverse isotropy with audhorizontal symmetry axis). The numerical modelling demonstrates the effects of fluidudviscosity on medium elastic properties and seismic reflectivity, as well as the possibilityudof using them to discriminate between oil and water saturation. Analysis of real dataudreveals that it is hard to use the P-wave to discriminate oil-water saturation. However,udcharacteristic shear-wave splitting behaviour due to pore pressure changes demonstratesudthe potential for discriminating between oil and water saturation in fractured reservoirs.
机译:自从1986年首次在油气储层中观测到地震各向异性以来,石油工业就已经认识到地震各向异性的重要性,从那时起,人们就一直在寻求将地震各向异性应用于解决地球物理问题。但是,仍然存在许多问题,这限制了该技术的应用。 ud如今,越来越多的具有宽方位角的3D多分量地震数据变得可用。这些为地震双各向异性的研究提供了更多的机会。本文主要研究在3D ud多分量地震数据中使用地震各向异性来表征地下裂缝,改善转换 udf成像和检测裂缝性储层中的流体含量,这些对于裂缝性储层勘探和监测都是重要的。 ud为了利用地震各向异性来表征地下裂缝系统,等效的 udmedium理论已经建立了地震各向异性与裂缝 udproperties之间的联系。数值模拟表明,PS转换波的径向分量的振幅和间隔超程时间可用于类似于P波的椭圆拟合,以推导裂缝超性质。但是,无论是P波还是PS波,都需要足够的偏移覆盖以揭示具有方位角的椭圆变化的特征。 ud与数值模拟相比,地震物理模拟为P和PS-的方位角变化提供了额外的见解。波浪属性及其与非断裂属性的联系。对地震物理模型数据的分析表明,偏移量与目标层深度的比(偏移深度比)是控制裂缝分析合适属性和方法选择的关键参数。偏移深度比从0.7到1.0较小的数据可能更适合于振幅分析;使用行进时间或速度分析需要大于ud1.0的较大偏移深度比,这可以帮助降低采集足迹和结构印记对结果的影响。多分量地震数据经常被噪声严重污染,这将限制在地震各向异性分析中的应用潜力。已经开发出一种减少 ud3D多分量地震数据中噪声的新方法,并被证明对提高数据质量非常有帮助。该方法可以自动识别和消除3D转换波地震数据中的强噪声,而对有用的反射 ud信号几乎没有干扰。 ud分量旋转通常是3D多分量地震 udanalysis中的常规过程。但是,这项研究表明,某些购置几何形状可能会发生不正确的旋转,并可能导致剪切波分裂分析中的错误。已开发出一种质量 udcontrol方法来确保正确执行此过程。 ud地震各向异性的存在会影响地震成像的质量,但 udtudy研究表明,影响的程度取决于数据类型和目标 uddepth。 VTI各向异性(具有垂直对称轴的横向各向同性) udon P波图像的影响要比PS波图像弱得多。各向异性效应随P波和PS波的深度而减小。实际数据示例表明,考虑到VTI各向异性后,叠前时间偏移处理后的PS波的总体图像质量已得到改善。改进主要在该部分的上部。ud监控流体分布是生产储层的重要任务。基于多尺度岩石物理学模型的合成研究表明,可以使用地震各向异性来获得HTI介质中的粘度信息(具有水平对称轴的横向各向同性)。数值模型证明了流体黏度对介质弹性和地震反射率的影响,以及利用它们区分油饱和度和水饱和度的可能性。实际数据分析表明,很难使用P波来区分油水饱和度。然而,由于孔隙压力的变化而具有的特征剪切波分裂行为证明了在裂缝性储层中区分油水饱和度的潜力。

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  • 作者

    Qian Zhongping;

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  • 年度 2010
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  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
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