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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Earth Science Institute, Slovak Academy of Sciences, Slovakia
2011-06-01
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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 |
work_keys_str_mv |
AT milanhvozdara theforwardproblemofmagnetometryfortheoblatespheroid AT janvozar theforwardproblemofmagnetometryfortheoblatespheroid AT milanhvozdara forwardproblemofmagnetometryfortheoblatespheroid AT janvozar forwardproblemofmagnetometryfortheoblatespheroid |
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