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Waveform inversion of poststacked reflection seismic data with well log constrained using nonlinear optimization methods

机译:非线性优化方法约束测井后叠加反射地震资料的波形反演

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Surface reflection seismic inversion techniques are currently applied by the industry for mapping the rock physical properties of oil reservoirs. This information permits speeding up the interpretation process to ultimately provide well locations. At present, many companies require the inversion to be completed before any well is drilled. Inversion techniques can be applied to prestacked and poststacked seismic data. Prestacked data inversion is more complex than poststacked, but it provides more information for the interpreter (e.g., P-wave and S-wave impedances). On the other hand, poststacked inversion provides only the acoustic P-wave impedance. However, the main outcome of prestacked inversion is the increase in resolution when full waveforms are inverted. Currently, poststacked seismic inversion is used to correlate P-wave impedance with rock physical properties obtained from well logs. The logs are provided by a well near the survey line, allowing images of different rock properties to be processed and analyzed. We extend the use of the acoustic P-wave impedance by constraining it with the well lithology, consequently categorizing the impedance by classes (i.e., sand, shale, and limestone) and converting the impedance to earth properties using well logs and regression models. This process allows us to build a single initial estimate of the earth property model, which is iteratively refined to produce a synthetic seismogram (by means ol forward modeling) to match the observed seismic data. The inversion algorithm that minimizes the misfits between observed and synthetic full-waveform data improves the P-wave velocity resolution. The interpreter can thus delineate thin channels (flow units saturated with hydrocarbons) that are undetected using current techniques.
机译:业界目前正在使用表面反射地震反演技术来绘制储油层的岩石物理特性图。该信息可以加快解释过程,最终提供井位。目前,许多公司要求在钻任何井之前先完成反演。反演技术可以应用于叠前和叠后的地震数据。叠前的数据反演比叠后的更为复杂,但是它为解释器提供了更多信息(例如,P波和S波阻抗)。另一方面,叠后反演仅提供声波阻抗。但是,叠前反演的主要结果是当全波形反演时分辨率提高。当前,叠后地震反演用于将P波阻抗与从测井获得的岩石物理特性相关联。测井资料由勘测线附近的一口井提供,可以处理和分析不同岩石性质的图像。我们通过将声波阻抗限制在井岩性上,从而扩展声波阻抗的使用范围,从而将阻抗按类别(即沙,页岩和石灰石)进行分类,并使用测井曲线和回归模型将阻抗转换为地球属性。这个过程使我们能够建立一个单独的地球属性模型的初始估计值,并对其进行迭代精炼以生成合成地震图(通过ol正向建模)来匹配观测到的地震数据。最小化观测到的和合成的全波形数据之间的失配的反演算法提高了P波速度分辨率。因此,解释器可以描绘出使用当前技术无法检测到的细通道(饱和烃流动单元)。

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