1887

Abstract

Full three-dimensional (3-D) inversion of magnetotelluric (MT) tensor has a great potential for the characterisation of complex geological structures at different scales. We developed a simple and robust 3D MT data inversion method based on the coarse-to-

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/content/papers/10.3997/2214-4609.201400136
2009-06-08
2021-12-09
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400136
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