2015
DOI: 10.1016/j.jcp.2014.12.041
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Identification of subsurface structures using electromagnetic data and shape priors

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Cited by 11 publications
(7 citation statements)
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References 53 publications
(81 reference statements)
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“…This mapping technique can increase the amount of information in the data set, particularly if the number of data is small [46]. The KPCA has already proven to be powerful as a preprocessing step for identification algorithms [47][48][49]. In this section, a brief description of KPCA for feature extraction is provided.…”
Section: Extracting Principal Components Based On Kpcamentioning
confidence: 99%
“…This mapping technique can increase the amount of information in the data set, particularly if the number of data is small [46]. The KPCA has already proven to be powerful as a preprocessing step for identification algorithms [47][48][49]. In this section, a brief description of KPCA for feature extraction is provided.…”
Section: Extracting Principal Components Based On Kpcamentioning
confidence: 99%
“…KPCA, as a novel nonlinear extension of PCA, extracts the principal exponents by using the kernel method. Although the actual meaning of the extracted principal components is not clear, KPCA has been already proven powerful as a preprocessing step for identification algorithms (Chen et al 2008;Mercer et al 2011;Tveit et al 2015). In this section, we provide a brief description of KPCA for feature extraction.…”
Section: Feature Selectionmentioning
confidence: 99%
“…While the joint-inversion techniques described above aim to utilize complementary data types in a single inversion process, so-called cooperative inversion techniques [55] aim to invert the data types in separate steps, with the resulting model from inversion of one data type acting as starting model or constraint for the subsequent inversion of another data type. Examples of cooperative inversion techniques can be found in [75,76], where interpreted seismic inversion results are used as structural prior information for CSEM inversion, and in [17,40,70], where inversion of each data type is done in sequence and, in some cases, iterated. Exchanging information between geophysical models in the disparate inversion sequences can be challenging, especially if the spatial resolutions of the data types are different.…”
Section: Introductionmentioning
confidence: 99%
“…We will apply a model-based parametrization to represent the unknown functions in the inversions. The particular model-based parameterization applied here (see, e.g., [7,76]) is based on the level-set framework, facilitating representation of region boundaries without a priori restrictions on their shapes. It is therefore well suited to represent the boundaries of the images of a large-scale CO 2 plume in the respective geophysical domains, that is, in the electric conductivity, density, and seismic velocity.…”
Section: Introductionmentioning
confidence: 99%