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Estimating seismic dispersion from prestack data using frequency-dependent AVO analysis 利用频率相关AVO分析从叠前数据估计地震频散
IF 0.5 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2010-01-01 DOI: 10.1190/1.3513759
Xiaoyang Wu, M. Chapman, Xiang-Yang Li
Recent laboratory measurement studies have suggested a growing consensus that fluid saturated rocks can have frequency-dependent properties within the seismic bandwidth. It is appealing to try to use these properties for the discrimination of fluid saturation from seismic data. In this paper, we develop a frequency-dependent AVO (FAVO) attribute to measure magnitude of dispersion from pre-stack data. The scheme essentially extends the Smith and Gidlow (1987)’s two-term AVO approximation to be frequency-dependent, and then linearize the frequency-dependent approximation with Taylor series expansion. The magnitude of dispersion can be estimated with least-square inversion. A high-resolution spectral decomposition method is of vital importance during the implementation of the FAVO attribute calculation. We discuss the resolution of three typical spectral decomposition techniques: the short term Fourier transform (STFT), continuous wavelet transform (CWT) and Wigner-Vill Distribution (WVD) based methods. The smoothed pseudo Wigner-Ville Distribution (SPWVD) method, which uses smooth windows in time and frequency domain to suppress cross-terms, provides higher resolution than that of STFT and CWT. We use SPWVD in the FAVO attribute to calculate the frequency-dependent spectral amplitudes from pre-stack data. We test our attribute on forward models with different time scales and crack densities to understand wave-scatter induced dispersion at the interface between an elastic shale and a dispersive sandstone. The FAVO attribute can determine the maximum magnitude of P-wave dispersion for dispersive partial gas saturation case; higher crack density gives rise to stronger magnitude of P-wave dispersion. Finally, the FAVO attribute was applied to real seismic data from the North Sea. The result suggests the potential of this method for detection of seismic dispersion due to fluid saturation.
最近的实验室测量研究表明,流体饱和岩石在地震带宽内可能具有频率依赖性。尝试利用这些性质从地震资料中区分流体饱和度是有吸引力的。在本文中,我们开发了一个频率相关的AVO (FAVO)属性来测量叠前数据的色散大小。该方案本质上是将Smith和Gidlow(1987)的两项AVO近似扩展为频率相关的,然后用泰勒级数展开对频率相关的近似进行线性化。用最小二乘反演可以估计色散的大小。在实现FAVO属性计算过程中,高分辨率的光谱分解方法至关重要。讨论了三种典型的光谱分解方法:短时傅里叶变换(STFT)、连续小波变换(CWT)和基于Wigner-Vill分布(WVD)的方法。平滑伪Wigner-Ville分布(SPWVD)方法利用时域和频域平滑窗口抑制交叉项,具有比STFT和CWT更高的分辨率。我们在FAVO属性中使用SPWVD从叠前数据中计算频率相关的频谱幅度。我们在不同时间尺度和裂缝密度的正演模型上测试了我们的属性,以了解弹性页岩和色散砂岩之间界面的波散射诱导色散。在色散部分气饱和情况下,FAVO属性可以确定p波色散的最大震级;裂纹密度越大,纵波频散强度越大。最后,将FAVO属性应用于北海实际地震资料。结果表明,该方法在检测流体饱和度引起的地震频散方面具有潜力。
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引用次数: 32
Predictive deconvolution by frequency domain Wiener filtering 预测反卷积的频域维纳滤波
IF 0.5 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2007-01-01 DOI: 10.1190/1.2792997
M. Broadhead, C. Liner, T. Ulrych
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引用次数: 1
Fusion Based Classification Method And Its Application 基于融合的分类方法及其应用
IF 0.5 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2007-01-01 DOI: 10.1190/1.2792784
Long Jin, Mrinal K. Sen, P. Stoffa
Summary Classification algorithms have many applications both in exploration and production seismology. Many classification algorithms have been reported in the literature, such as, seismic facies identification, lithology/fluid prediction, etc. However, improper choice of an algorithm and parameters for a specific problem will create incorrect classification results. Here, we elaborate on some of these issues. Further, we propose combing multiple classifiers with DempsterShafer theory (DS) to increase the accuracy of the classification. The philosophy of our approach is that different classifiers may offer complementary information about the patterns to be classified, combining classifiers in an efficient way can achieve better classification results than any single classifier. The effectiveness of this method is demonstrated with a synthetic data test.
分类算法在勘探和生产地震学中都有广泛的应用。文献中已经报道了许多分类算法,如地震相识别、岩性/流体预测等。然而,针对特定问题选择不当的算法和参数会产生错误的分类结果。在这里,我们详细阐述其中的一些问题。进一步,我们提出结合DempsterShafer理论(DS)对多个分类器进行组合,以提高分类的准确率。我们方法的理念是,不同的分类器可以提供关于要分类的模式的互补信息,以有效的方式组合分类器可以获得比任何单一分类器更好的分类结果。通过综合数据试验验证了该方法的有效性。
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引用次数: 4
Estimation of effective pressure and water saturation by viscoelastic inversion of synthetic time-lapse seismic data for a gas sandstone reservoir 含气砂岩储层时移合成地震资料粘弹性反演有效压力和含水饱和度
IF 0.5 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2005-01-01 DOI: 10.1190/1.2148220
U. Tiwari, G. McMechan
Summary Inversion of synthetic seismic data for a viscoelastic reservoir model produces estimates of changes in effective pressure (Pe) and water saturation (Sw). Application is to analysis of time-lapse seismic data for a gas sandstone reservoir. To generate synthetic time-lapse viscoelastic seismic data, reservoir properties [porosity (�-), clay content, permeability (k), Pe and Sw] are used to define the corresponding viscoelastic seismic properties [compressional and shear velocities (Vp and Vs), density (�! ) and compressional and shear quality factors (Qp and Qs)] using petro-seismic modeling. It is assumed that porosity, clay content and permeability do not change during production and are known. Full wavefield inversion is performed for different production scenarios, on synthetic viscoelastic time-lapse seismic data, using a grid search refined by a conjugate gradient solution. Estimation of unique values of Pe and Sw from two independent data (such as Vp/Vs and Qs/Qp) is feasible, if the other reservoir properties are known. Noisy data produces a range of solution values. The composite effect of ®Pe and ®Sw is approximately equal to the sum of the two separate effects. Seismic time-lapse changes are less sensitive to the pressure change than to changes in saturation. For the reservoir properties (�- , clay content, k), and the dominant seismic frequency used in the example, �! and Qs/Qp are most sensitive to Sw, Vp is most sensitive to Pe, and Vs, Qp and Qs and Vp/Vs are sensitive to both Sw and Pe.
对粘弹性储层模型的合成地震数据进行反演,可以估算出有效压力(Pe)和含水饱和度(Sw)的变化。应用于某含气砂岩储层时移地震资料分析。为了生成合成时移粘弹性地震数据,利用储层性质[孔隙度(-)、粘土含量、渗透率(k)、Pe和Sw]来定义相应的粘弹性地震性质[纵波和剪切速度(Vp和Vs)、密度(- !)]。以及挤压和剪切质量因子(Qp和Qs)]。假设孔隙度、粘土含量和渗透率在生产过程中不变,并且是已知的。利用共轭梯度解改进的网格搜索,对合成粘弹性时移地震数据进行了不同生产场景下的全波场反演。如果已知其他储层性质,则可以通过两个独立数据(如Vp/Vs和Qs/Qp)估算出Pe和Sw的唯一值。有噪声的数据产生一系列的解值。®Pe和®Sw的复合效应近似等于两种单独效应的总和。地震时移变化对压力变化的敏感性低于对饱和度变化的敏感性。对于储层性质(-,粘土含量,k),以及示例中使用的主要地震频率,- !Qs/Qp对Sw最敏感,Vp对Pe最敏感,Vs、Qp、Qs和Vp/Vs对Sw和Pe都敏感。
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引用次数: 0
Multiple Attenuation In the Plane Wave Domain By Match Filtering 基于匹配滤波的平面波域多重衰减
IF 0.5 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 1999-01-01 DOI: 10.1190/1.1820807
R. Pestana, P. Stoffa, Mrinal K. Sen
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引用次数: 1
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Journal of Seismic Exploration
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