首页> 外文会议>SEG Houston 2013 >Prestack waveform inversion of four-component, two-azimuth surface seismic data for orthorhombic elastic media parameters using a nondominated sorting genetic algorithm
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Prestack waveform inversion of four-component, two-azimuth surface seismic data for orthorhombic elastic media parameters using a nondominated sorting genetic algorithm

机译:三组分的Prestack波形反转,双方形弹性介质参数使用NondoMinated分类遗传算法

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Consideration of azimuthal anisotropy, at least to an orthorhombic symmetry is important in exploring the naturally fractured and unconventional hydrocarbon reservoirs. Inverting surface seismic data for subsurface orthorhombic properties is however a challenge. Such an inversion- needs multicomponent seismic data requiring inversion algorithms capable of simultaneously optimizing multiple objectives, one for each data component. In addition, an accurate extraction of subsurface azimuthal anisotropy requires multicomponent seismic data acquired at a fine spatial resolution along many source-to-receiver azimuthal orientations. Because routine acquisition of such-data is prohibitively expensive, they are typically available for two or at most three azimuthal orientations at a spatial resolution where such an inversion could be applied. In this work, we apply a multiobjective optimization method using a nondominated sorting genetic algorithm to extract the anisotropic elastic properties and density from multicomponent surface seismic data sorted along two different source-to-receiver azimuthal orientations that extracted the rotated elastic properties along these directions. We then use the extracted models along two azimuths and the azimuthal angle difference between them to construct the orthorhombic elastic properties of the subsurface. Applying our methodology on a multilayered model with different anisotropic symmetries, we demonstrate that our method is capable of extracting most of the elastic parameters and density to a reasonable accuracy. We conclude that inverting surface seismic data along two azimuths and then combining them into an orthorhombic subsurface model is a practical way to characterize the subsurface for azimuthal anisotropy
机译:对方位角各向异性的考虑,至少对勘探天然骨折和非传统的烃储层非常重要。然而,反相表面地震数据对于地下正交性能是挑战。这种反演需要多组分地震数据,需要能够同时优化多个目标的反转算法,每个数据组件一个。此外,准确提取地下方位调各向异性需要沿着许多源到接收方向方向上以精细空间分辨率获取的多组分地震数据。因为常规获取这种数据的诸如昂贵的,所以它们通常可用于两个或大多数三方位角,其空间分辨率,其中可以应用这种反转。在这项工作中,我们使用非目标分选遗传算法应用多目标优化方法,以从沿着两个不同的源 - 接收方向方向排序的多组分表面地震数据的各向异性弹性特性和密度,其沿着这些方向提取旋转的弹性特性。然后,我们沿着两个方位角和它们之间的方位角差来使用提取的模型来构造地下的正极弹性特性。在具有不同各向异性对称的多层模型上应用我们的方法,我们证明我们的方法能够以合理的精度提取大部分弹性参数和密度。我们得出结论,沿着两个方位角反转表面地震数据,然后将它们组合成正交地下模型是表征外表面的实用方式,用于方位角各向异性

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