Advancements in Magnetic Field Methods and Natural Resources Exploration

A special issue of Geosciences (ISSN 2076-3263). This special issue belongs to the section "Geophysics".

Deadline for manuscript submissions: closed (30 September 2020) | Viewed by 3796

Special Issue Editors


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Guest Editor
Department of Earth, Environment and Resources Science, University Federico II, Complesso di Monte S. Angelo, Via Cintia, Edifice L, 80126 Naples, Italy
Interests: applied geophysics; potential field data analysis and modeling; remote sensing
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Guest Editor
Geologische Bundesanstalt, Vienna, Austria
Interests: airborne electromagnetics; geophysical measurements; coastal karst system

Special Issue Information

Dear Colleagues,

Geophysical exploration methods play a key role in natural resources studies. The role of these methods is to provide valuable information on the type, shape, size, and depth of the geological structures constituting the natural-resources reservoirs. They also yield information on the geometry and type of fractures where oil, gasses, water and geothermal fluids circulate.

Magnetic exploration methods provide insights for a better understanding of the geologic, structural and geothermal characteristics of an area. This is particularly true for volcanic and sedimentary zones, where recent deposits often cover important structures. In those cases, magnetic methods can locate buried structures such as lineaments, faults, reservoirs and magmatic structures. This is possible thanks to the existence of susceptibility contrasts between the cover soil and the buried structures that often causes detectable anomalies.

In past decades, magnetic surveying had become popular as one of the most effective techniques supporting seismic methods in natural resources exploration. Indeed, magnetic methods are now standard in the pre-drilling phase to identify areas of interest and estimate size and location of reservoirs.

Innovation involves the development of new measurement techniques, including new instruments, new interpretative methods (analysis, imaging and inversion of data, including large scale methods) and new areas of exploration such as Deep-Sea Mining.

Recently, great advances were made in signal enhancement and edge analysis of potential field anomalies, thanks to methods allowing a suitable differentiation of the field without making the process unstable. New three-dimensional (3D) imaging techniques provide an estimate of the magnetization distribution within the underground by means of high-resolution images of the source distribution. Most of these methods are fast and reliable in the presence of shallow and compact sources. In the presence of deep/complex sources, the resolution of the intepretative models is reduced. Nevertheless, great effort was spent by the scientific community to overcome problems causing low signal-to-noise ratio in the measurements and to improve depth resolution in the quantitative interpretation of magnetic souces.

The aim of this Special Issue of Geosciences is to showcase the latest developments in the field of exploration of natural resources by magnetic methods, with emphasis on advancements in exploration and interpretation techniques. We specifically invite contributions addressing the following aspects:

  • Methods for Magnetic Data Processing included Noise Removal;
  • Methods for Signal Enhancement;
  • Imaging and Inversion Techniques;
  • Significant Case Studies in Natural Resources Exploration (oil, gas, water, geothermal reservoirs).

Dr. Valeria Paoletti
Mag. Ingrid Schattauer
Guest Editors

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Keywords

  • Advanced Processing and Interpretation Methods for Magnetometric Data
  • Noise Removal Techniques
  • Signal Enhancement and Source Edge Detection Methods
  • 3D Imaging and Inversion for Natural Resources Exploration

Published Papers (1 paper)

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14 pages, 4106 KiB  
Article
Global High-Resolution Magnetic Field Inversion Using Spherical Harmonic Representation of Tesseroids as Individual Sources
by Eldar Baykiev, Dilixiati Yixiati and Jörg Ebbing
Geosciences 2020, 10(4), 147; https://doi.org/10.3390/geosciences10040147 - 16 Apr 2020
Cited by 6 | Viewed by 3359
Abstract
In this study, we present a novel approach combining the advantages of tesseroids in representing geophysical structures though their voxel-like discretization features with a spherical harmonic representation of the magnetic field. Modelling of the Earth lithospheric magnetic field is challenging since part of [...] Read more.
In this study, we present a novel approach combining the advantages of tesseroids in representing geophysical structures though their voxel-like discretization features with a spherical harmonic representation of the magnetic field. Modelling of the Earth lithospheric magnetic field is challenging since part of the spectra is hidden by the core field and the forward modeled field of a lithospheric magnetization is always biased by the spectral range used. In our approach, a spherical harmonic representation of the magnetic field of spherical prisms (tesseroids) is used for high-resolution magnetic inversion of lithospheric field models. The use of filtered spherical harmonic models of the magnetic field of each tesseroid ensures that the resulting field matches the spectral range of the input data. For the inversion, we use the projected gradient method. The projected gradient method easily allows us to assign an initial guess (i.e., a-priori assumption) for the inversion and avoids negative values of susceptibilities. The latter is providing more plausible models since induced magnetization is assumed to be dominant over the continents and, for the oceans, a remanence model can be subtracted. We show an application of the technique to a synthetic dataset and a satellite-derived lithospheric field model where the model geometry is based on seismic information. We also demonstrate a proof-of-concept for high-resolution tile-wise inversion for the Bangui anomaly in Africa. Full article
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