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3D gravity inversion with Euler deconvolution as a priori information

机译:以Euler反卷积为先验信息的3D重力反演

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摘要

It is difficult to obtain high-resolution images by 3D gravity inversion, because the problem is extremely underdetermined - there are too many model parameters. In order to reduce the number of model parameters we propose a 3D gravity inversion scheme utilising Euler deconvolution as a priori information. The essential point of this scheme is the reduction of the nonuniqueness of solutions by restricting the inversion space with the help of Euler deconvolution. We carry out a systematic exploration of the growing body process, but only in the restricted space within a certain radius of the Euler solutions. We have tested our method with synthetic gravity data, and also applied it to a real dataset, to delineate underground cavities in a limestone area. We found that we obtained a more reasonable subsurface density image by means of this combination between the Euler solution and the inversion process.
机译:通过3D重力反演很难获得高分辨率的图像,因为该问题非常不确定-模型参数太多。为了减少模型参数的数量,我们提出了一种利用欧拉反卷积作为先验信息的3D重力反演方案。该方案的要点是借助Euler反卷积来限制反演空间,从而减少解的非唯一性。我们对生长过程进行了系统的探索,但仅在欧拉解的一定半径内的受限空间内进行。我们已经使用合成重力数据测试了我们的方法,并将其应用于真实数据集,以描绘石灰岩地区的地下洞穴。我们发现,通过欧拉解和反演过程之间的这种组合,我们获得了更合理的地下密度图像。

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