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Potential theory in gravity and magnetic applications

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TLDR
In this article, the potential of the geomagnetic field has been studied in vector calculus, and the results of the potential have been shown to be equivalent to the conversion of units.
Abstract
Introduction 1. The potential 2. Consequences of the potential 3. Newtonian potential 4. Magnetic potential 5. Magnetization 6. Spherical harmonic analysis 7. Regional gravity fields 8. The geomagnetic field 9. Forward method 10. Inverse method 11. Fourier-domain modeling 12. Transformations A. Review of vector calculus B. Subroutines C. Review of sampling theory D. Conversion of units.

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Interpretation of gravity anomalies to delineate some structural features of Biga and Gelibolu peninsulas, and their surroundings (north-west Turkey)

TL;DR: In this paper, derived anomaly traces were presented for the interpretation of some shallow structural features of Biga and Gelibolu peninsulas using a MATLAB-based software package (Gravity and Magnetic Interpretation - GMINTERP).
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Crustal Structure of Turkey from Aeromagnetic, Gravity and Deep Seismic Reflection Data

TL;DR: A reduction to pole (RTP) map of aeromagnetic and gravity anomalies obtained from the General Directorate of Mineral Research and Exploration were subjected to upward continuation to 3 km from the ground surface to suppress shallow effects and to expose only regional, deep sources as mentioned in this paper.
Journal ArticleDOI

Geological mapping of Jharia Coalfield, India using GRACE EGM2008 gravity data: a vertical derivative approach

TL;DR: In this article, high-resolution satellite gravity data of gravity recovery and climate experiment (GRACE) generated by Earth Gravity Model-2008 (EGM2008) have been used for geological mapping of the Jharia coalfield.
Journal ArticleDOI

Study of impact demagnetization at Mars using Monte Carlo modeling and multiple altitude data

TL;DR: In this article, the authors present a framework for determining the effects on the magnetic field signatures of large demagnetized impact basins on Mars, due to the dominant direction, strength, thickness, and vertical and horizontal coherence wavelengths of the surrounding crustal magnetization.
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