The forward problem of magnetometry for the oblate spheroid

We present analytical solution of the forward magnetometric problem for the oblate spheroid (rotational ellipsoid) as a causative body. The shorter semiaxis of the ellipsoid is supposed to be vertical to the surface of the earth. There is proved that the uniform inducing magnetic field B0 induces in...

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Main Authors: Milan HVOŽDARA, Ján VOZÁR
Format: Article
Language:English
Published: Earth Science Institute, Slovak Academy of Sciences, Slovakia 2011-06-01
Series:Contributions to Geophysics and Geodesy
Subjects:
Online Access:https://journal.geo.sav.sk/cgg/article/view/51
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spelling doaj-f140fb0ab9664984b03eb9f78e23dfdd2020-11-25T04:10:48ZengEarth Science Institute, Slovak Academy of Sciences, SlovakiaContributions to Geophysics and Geodesy1338-05402011-06-0141215917710.2478/v10126-011-0006-z51The forward problem of magnetometry for the oblate spheroidMilan HVOŽDARA0Ján VOZÁR1Geophysical Institute of the Slovak Academy of SciencesGeophysical Institute of the Slovak Academy of SciencesWe present analytical solution of the forward magnetometric problem for the oblate spheroid (rotational ellipsoid) as a causative body. The shorter semiaxis of the ellipsoid is supposed to be vertical to the surface of the earth. There is proved that the uniform inducing magnetic field B0 induces inside the spheroid also uniform magnetic field but its modulus and direction are different as compared to B0. The isolines and profile curves of ΔZ and ΔT are calculated on the plane z = const above the ellipsoid, as well as on the surface of the hill in the shape of cutted cone.https://journal.geo.sav.sk/cgg/article/view/51geophysical magnetometry, potential due to oblate spheroid, magnetic anomalies due to magmatic bodies
collection DOAJ
language English
format Article
sources DOAJ
author Milan HVOŽDARA
Ján VOZÁR
spellingShingle Milan HVOŽDARA
Ján VOZÁR
The forward problem of magnetometry for the oblate spheroid
Contributions to Geophysics and Geodesy
geophysical magnetometry, potential due to oblate spheroid, magnetic anomalies due to magmatic bodies
author_facet Milan HVOŽDARA
Ján VOZÁR
author_sort Milan HVOŽDARA
title The forward problem of magnetometry for the oblate spheroid
title_short The forward problem of magnetometry for the oblate spheroid
title_full The forward problem of magnetometry for the oblate spheroid
title_fullStr The forward problem of magnetometry for the oblate spheroid
title_full_unstemmed The forward problem of magnetometry for the oblate spheroid
title_sort forward problem of magnetometry for the oblate spheroid
publisher Earth Science Institute, Slovak Academy of Sciences, Slovakia
series Contributions to Geophysics and Geodesy
issn 1338-0540
publishDate 2011-06-01
description We present analytical solution of the forward magnetometric problem for the oblate spheroid (rotational ellipsoid) as a causative body. The shorter semiaxis of the ellipsoid is supposed to be vertical to the surface of the earth. There is proved that the uniform inducing magnetic field B0 induces inside the spheroid also uniform magnetic field but its modulus and direction are different as compared to B0. The isolines and profile curves of ΔZ and ΔT are calculated on the plane z = const above the ellipsoid, as well as on the surface of the hill in the shape of cutted cone.
topic geophysical magnetometry, potential due to oblate spheroid, magnetic anomalies due to magmatic bodies
url https://journal.geo.sav.sk/cgg/article/view/51
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