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Joint inversion of marine MT and wide aperture seismic data using a 'hybrid'-based approach

机译:使用“混合的方法”的海洋MT和宽孔径地震数据的联合反演

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We present a 'hybrid'-based workflow for the joint inversion of marine Magnetotelluric (MT) and wide aperture seismic data that reconstructs the velocities, resistivities and shapes within regions of interest (ROI) using an 'image'-based inversion approach followed by a 'structure'-based inversion algorithm where the ROI are parameterized using both surfaces and bodies for localized targeting and rapid inversion. This workflow preserves the velocity and resistivity structure already arrived at, enabling the integration of geology in the geophysical process. The 'structure'-based inversion allows for: faster velocities and resistivities model building, targeting salt bodies, focusing on geobodies. We show that the reconstructed velocities, resistivities and shapes of ROI are consistent with both the MT and the seismic data and that considerable improvement in resolution and speed is achieved compared to the current state-of-the-art. We illustrate the advantages and drawbacks of the 'hybrid' inversion using synthetic data.
机译:我们为船用磁通镜(MT)的联合反演提供了一个“混合的工作流程,并且使用”基于图像的反转方法“之后,重建感兴趣区域(ROI)内的速度,电阻和形状的宽孔径地震数据基于结构的反转算法,其中ROI使用曲面和主体参数化,用于本地化目标和快速反转。该工作流程保留了已经到达的速度和电阻率结构,从而能够在地球物理过程中集成地质。 “基于结构的反演允许:更快的速度和电阻模型建筑物,瞄准盐体,重点在地质上。我们表明,ROI的重建速度,电阻和形状与MT和地震数据一致,与当前最先进的最先进相比,实现了分辨率和速度的显着提高。我们说明了使用合成数据的“混合动力”反演的优点和缺点。

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