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A Seismic Reservoir Characterization Work Flow for Reducing Risk Utilizing AVO, Simultaneous Prestack Inversion, and Rock Physics

机译:用于降低风险的地震储层特征工作流程利用AVO,同时提取物倒置和岩石物理学

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In this paper, an integrated seismic-based reservoir characterization, work. flow is presented which includes fluid substitution, AVO modeling, prestack simultaneous inversion, and lithology and petrophysi-cal property prediction. Forward modeling is normally the most effective way to commence an AVO analysis, which begins with determining the fluid response by calculating seismic velocity and offset-dependant reflectivity changes due to different fluid saturations. The investigation of amplitude variations with offset seeks to extract information about the reservoir rock by measuring changes in amplitude with varying incident angle. Next, the seismic data are analyzed in order to determine whether a conditioning process must be implemented to extract the most out of the seismic data. The aim is to preserve the AVO response while flattening events as much as possible as well as adequately attenuating noise without generating artifacts. Prestack simultaneous AVO inversion follows seismic conditioning, where the data are converted from interface properties to layer properties by the use of a global optimization algorithm with a nonlinear cost function to simultaneously invert a number of input stacks to an earth model. The final process in the characterization work flow is determining a spatial distribution of lithology and petrophysical properties based on rock physics and Bayesian statistics using the acoustic and elastic output volumes from the simultaneous inversion.
机译:在本文中,一个完整的基于地震油藏描述工作。流被呈现,其包括流体置换,AVO模拟,叠前同步反演,和岩性和petrophysi-CAL性能预测。正演模拟通常是开始一个AVO分析,这与确定通过计算地震速度,并且由于不同的流体饱和度偏移依赖性反射率变化的流体响应开始的最有效途径。振幅变化的与偏移调查寻求通过测量振幅变化具有不同的入射角以提取关于储层岩石的信息。接着,将地震数据,以确定一个调节过程是否必须被执行,以提取最有效地对地震数据的分析。其目的是保持AVO响应,而平坦化事件尽可能以及充分噪声衰减而不产生伪像。叠前同步AVO反演地震如下空调,其中,所述数据被从接口属性通过使用全局优化算法的同时转化成层性能具有非线性成本函数来反转一批输入堆栈至一个地球模型。在表征工作流程的最后程序确定基于使用声波和弹性输出量从同步反演岩石物理和贝叶斯统计岩性和岩石物理性质的空间分布。

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