K. Spitzer, OBSERVATIONS OF GEOMAGNETIC-PULSATIONS AND VARIATIONS WITH A NEW BOREHOLE MAGNETOMETER DOWN TO DEPTHS OF 3000-M, Geophysical journal international, 115(3), 1993, pp. 839-848
A triaxial magnetometer has been developed for investigating the in si
tu skin effect of horizontal geomagnetic pulsations and variations in
deep boreholes. The observations were carried out in the pilot borehol
e of the Continental Deep Drilling Program of Germany (KTB) down to de
pths of 3000 m and up to temperature of 90-degrees-C. A weak skin effe
ct, due to the known very low conductivity of the penetrated crystalli
ne rocks, of 90 to 95 per cent in amplitude and -5-degrees to -10-degr
ees rotation in phase has been observed at periods of 10 s and magneto
meter depth of 2400 m. An essential prerequisite for all calculations
is the accurate determination of the orientation of the downhole magne
tometer. It is demonstrated how oriented record samples of temporal va
riations at depth correlate precisely with those from the surface. Res
ults from surface magnetotelluric (MT) investigations show strong loca
l distortions of the telluric field. The distortion of the MT tensor r
esponse has been determined by means of newly introduced skin-effect t
ransfer functions, which are assumed to be undistorted.