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Telluric measurements and differential geomagnetic soundings in the Rhinegraben (period range: 1–125 s)
Author(s) -
Alboliy Y.,
Fabriol H.
Publication year - 1981
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1981.tb02702.x
Subject(s) - earth's magnetic field , geology , geophysics , anomaly (physics) , magnetic field , geodesy , period (music) , magnetic anomaly , range (aeronautics) , seismology , physics , condensed matter physics , materials science , quantum mechanics , acoustics , composite material
Summary. In 1976, seven stations measuring the variations of the telluric and geomagnetic fields in the period range 1–125 s were operated in the southern part of the Rhinegraben. The study of the recordings shows that the telluric field is linearly polarized according to a direction perpendicular to that of the horizontal anomalous magnetic fields and that telluric and anomalous magnetic fields have the same time dependence. The conducted currents responsible for the anomaly flow probably into the superficial conductive layer.

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