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    • 7. 发明授权
    • Method for obtaining porosity and shale volume from seismic data
    • 从地震数据中获取孔隙度和页岩体积的方法
    • US08126651B2
    • 2012-02-28
    • US11922815
    • 2006-06-06
    • Rebecca L. SaltzerChristopher J. FinnRongrong Lu
    • Rebecca L. SaltzerChristopher J. FinnRongrong Lu
    • G01V1/00G01V1/28
    • G01V1/306
    • Method for obtaining rock parameters such as porosity and vshale directly from inversion of seismic data corresponding to a single trace location. This method is distinguished from existing methods that obtain elastic properties from inversion of seismic data, then relate the elastic parameters to rock lithology parameters such as porosity or vshale because it is accomplished in one step, can incorporate anisotropy and does not require multiple trace locations for stability. The data are separated into partial stacks, and a wavelet is specified for each stack. A set of linearized equations are constructed relating seismic reflectivity to changes in elastic parameters, and another set of linearized equations is constructed relating the changes in elastic parameters to the lithologic parameters. The linearized reflectivity equations are combined with the linearized rock physics equations, convolved with the specified wavelets, and equated to the seismic data. The resulting matrix equations are then inverted and a solution is obtained for all offsets simultaneously.
    • 直接从对应于单一轨迹位置的地震数据反演获得岩石参数如孔隙度和垂直叶片的方法。 该方法与从地震数据反演获得弹性性质的现有方法不同,然后将弹性参数与岩石岩性参数(如孔隙度或vshale)相关联,因为它在一个步骤中完成,可以包含各向异性,并且不需要多个迹线位置 稳定性。 数据被分成部分堆栈,并为每个堆栈指定一个小波。 构造了一组线性方程,将地震反射率与弹性参数的变化相关联,另外建立了一组线性化方程,将弹性参数的变化与岩性参数相关联。 线性化反射率方程与线性化岩石物理方程组合,与指定的小波卷积,并等同于地震数据。 然后将所得到的矩阵方程反相,同时获得所有偏移的解。
    • 8. 发明申请
    • Method for Obtaining Porosity and Shale Volume From Seismic Data
    • 从地震数据中获取孔隙度和页岩体积的方法
    • US20090271118A1
    • 2009-10-29
    • US11922815
    • 2006-06-06
    • Rebecca L. SaltzerChristopher J. FinnRongrong Lu
    • Rebecca L. SaltzerChristopher J. FinnRongrong Lu
    • G01V1/28
    • G01V1/306
    • Method for obtaining rock parameters such as porosity and vshale directly from inversion of seismic data corresponding to a single trace location. This method is distinguished from existing methods that obtain elastic properties from inversion of seismic data, then relate the elastic parameters to rock lithology parameters such as porosity or vshale because it is accomplished in one step, can incorporate anisotropy and does not require multiple trace locations for stability. The data are separated into partial stacks, and a wavelet is specified for each stack. A set of linearized equations are constructed relating seismic reflectivity to changes in elastic parameters, and another set of linearized equations is constructed relating the changes in elastic parameters to the lithologic parameters. The linearized reflectivity equations are combined with the linearized rock physics equations, convolved with the specified wavelets, and equated to the seismic data. The resulting matrix equations are then inverted and a solution is obtained for all offsets simultaneously.
    • 直接从对应于单一轨迹位置的地震数据反演获得岩石参数如孔隙度和垂直叶片的方法。 该方法与从地震数据反演获得弹性性质的现有方法不同,然后将弹性参数与岩石岩性参数(如孔隙度或vshale)相关联,因为它在一个步骤中完成,可以包含各向异性,并且不需要多个迹线位置 稳定性。 数据被分成部分堆栈,并为每个堆栈指定一个小波。 构造了一组线性方程,将地震反射率与弹性参数的变化相关联,另外建立了一组线性化方程,将弹性参数的变化与岩性参数相关联。 线性化反射率方程与线性化岩石物理方程组合,与指定的小波卷积,并等同于地震数据。 然后将所得到的矩阵方程反相,同时获得所有偏移的解。