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Using Seismic Full Waveform Inversion to Guide 1D Marine CSEM Inversions for Resolving Multiple Resistive Layers

机译:使用地震全波形反转来引导1D船用CSEM反转,用于解析多个电阻层

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In order to study the physical processes occurring inside the earth we require accurate images of the subsurface. Two of the most successful methods for doing this are seismic and electromagnetic sensing, but no current single method is entirely sufficient for building a complete picture. This problem is especially acute in industrial applications such as hydrocarbon reservoir permanent monitoring, where some changes in reservoir fluid properties are near impossible to detect with conventional acoustic seismics. Electromagnetic methods can detect the fluid properties of interest however the resolution is poor. We present a method which uses the resolution at depth of full waveform seismic inversion to guide a controlled source electromagnetic inversion. The result of combining the techniques in this manner on synthetic examples allows us to model multiple layered structure to within a few percent of the true values.
机译:为了研究地球内部发生的物理过程,我们需要准确的地下图像。这两种最成功的方法是地震和电磁感测,但没有目前的单一方法完全足以建立完整的画面。该问题在碳氢化合物储层永久监测之类的工业应用中特别急剧,其中储层液性能的一些变化近不可能用常规声学地震检测。电磁方法可以检测感兴趣的流体性质然而分辨率差。我们介绍了一种方法,该方法在完全波形地震逆转深度使用分辨率来引导受控源电磁反转。以这种方式对合成示例组合技术的结果允许我们将多个分层结构模拟到真实值的百分比内。

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