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Subsurface model prediction using a neural network- a real data example from the Rock-Springs uplift, Wyoming

机译:地下模型预测使用神经网络 - 来自摇滚弹簧隆起的真实数据示例,Wyoming

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Seismic inversion is a method which extracts seismic attributes such as the P- and S-wave velocities, density, acoustic impedance, Poison's ratio etc. from seismic data, which in turn, provide the subsurface rock physics i.e., the reservoir attributes such as porosity, permeability, lithology etc. Conventional model based inversions, such as Prestack waveform inversion (PWI), simultaneous amplitude-variation-with-offset (AVO) inversion, use theoretical relationships between model parameters and observed seismic data that are based upon some assumptions. All these methods predict the subsurface earth model to an accuracy to which the underlying theoretical relationships are valid. In this paper we present a new approach of seismic inversion methodology, which is a data driven methodology (Schultz et al., 1994), and uses statistical approach rather than deterministic method to predict the subsurface reservoir properties. This method combines neural net inversion with PWI in a hybrid methodology. Applying our method to the Rock-Springs uplift (RSU) real seismic data and comparing with AVO inversion, we demonstrate that our method provides a comparable image to that from AVO inversion.
机译:地震反演是一种从地震数据中提取诸如P型和S波速度,密度,声阻抗,毒药的比例等的地震属性的方法,这反过来又提供了地下岩石物理学,即储层属性,如孔隙率,渗透性,岩性等传统基于模型的反转,如Prestack波形反转(PWI),同时幅度变化 - 偏移(AVO)反转,使用模型参数之间的理论关系和观察基于一些假设的地震数据。所有这些方法将地下地球模型预测到底层理论关系有效的准确性。在本文中,我们提出了一种新的地震反演方法方法,这是一种数据驱动方法(Schultz等,1994),并使用统计方法而不是确定性方法来预测地下储层性质。该方法将神经净反转与PWI以混合方法结合起来。将我们的方法应用于Rock-Springs Uplift(RSU)真实地震数据并与AVO反转进行比较,我们证明我们的方法从AVO反转提供了与此相当的图像。

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