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Potential theory in gravity and magnetic applications
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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.read more
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Inland extent of the Weddell Sea Rift imaged by new aerogeophysical data
Tom A. Jordan,Fausto Ferraccioli,Neil Ross,Hugh F. J. Corr,Philip T. Leat,Robert Bingham,David M. Rippin,Anne M. Le Brocq,Martin J. Siegert +8 more
TL;DR: Aerogeophysical data over the catchments of Institute and Moller ice streams reveal the inland extent of the Weddell Sea Rift against the Ellsworth-Whitmore block and a hitherto unknown major left-lateral strike slip boundary between East and West Antarctica as mentioned in this paper.
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Central magnetic anomalies of Nectarian-aged lunar impact basins: Probable evidence for an early core dynamo
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Curie point depths of Bulgarian territory inferred from geomagnetic observations and its correlation with regional thermal structure and seismicity
TL;DR: In this article, the basal depth of the magnetic layer (Curie point depths) of Bulgarian territory was calculated using geomagnetic field observation and the variations of this border were mapped for the first time.
Shell Thickness Variations and the Long Wavelength Topography of Titan
Francis Nimmo,Bruce G. Bills +1 more
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Magnetic field transforms with low sensitivity to the direction of source magnetization and high centricity
Petar Stavrev,Daniela Gerovska +1 more
TL;DR: In this paper, the authors proposed transforms based on differential operators such as the gradient of T and its modulus R, the Laplacian L, the product T∇2T and its square root Q, and the L 2 ∇2(T2) and the square root E, to estimate the influence of the magnetization direction.