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Joint inversion of seismic and electric data applied to 2D media

机译:应用于2D介质的地震数据和电数据的联合反演

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摘要

Methods based on the seismic P-wave, seismic surface wave, and apparent resistivity are commonly used in the solution of several near-surface problems. However, the solution nonuniqueness and the intrinsic limitations of these methods can cause inconsistency in the final results. Dispersion curves of surface waves, P-wave traveltimes, and apparent-resistivity data were jointly inverted to obtain internally consistent and more reliable final model of P- and S-wave velocities and resistivity. A collection of 1D layered models was obtained by a deterministic joint inversion algorithm based on the laterally constrained inversion scheme. The three data sets were jointly inverted imposing the same structure and Poisson's ratio was introduced as a physical link between P- and S-wave velocities to better constrain the inversion. No physical link was imposed between the resistivity and the seismic velocities. The inversion algorithm was tested on synthetic data and then applied to a field case, where benchmark borehole data were available. The synthetic and field examples provided results in agreement with the true model and the existing geologic information, respectively.
机译:解决几个近地表问题时,通常使用基于地震P波,地震地表波和视电阻率的方法。但是,这些方法的解唯一性和固有局限性可能导致最终结果不一致。联合反转表面波的色散曲线,P波传播时间和视电阻率数据,以获得内部一致且更可靠的P波和S波速度和电阻率的最终模型。通过基于横向约束反演方案的确定性联合反演算法,获得了一维分层模型的集合。将这三个数据集共同反转以施加相同的结构,并引入泊松比作为P波和S波速度之间的物理链接,以更好地限制反演。在电阻率和地震速度之间没有施加物理联系。该反演算法在合成数据上进行了测试,然后应用于具有基准井眼数据的现场案例。综合实例和现场实例提供的结果分别与真实模型和现有地质信息一致。

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