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  • 1
    Publication Date: 1965-01-01
    Description: The first part of this paper describes the investigation of thermomagnetic effects inthree basalt samples. It was found that when a sample was heated in air the ferrimagnetic mineral component changed from a homogeneous member of the Ulvöspinell-Magnetite-series into two components. One of these had the same 0/Fe-ratio, the other one the same Fe/Ti-ratio as the original mineral. No changes took place when the sample was heated in a vacuum of 10-5 Torr. The second part deals with the observation of domain patterns in natural magnetites and the changes of these patterns under the influence of external magnetic fields. With the help of a new polishing technique powder patterns could be observed on magnetite grains in a non-conducting rock matrix. In the third part the magnetization of the Suevites-that are tuffaceous rocks formed in connection with the formation of the Ries crater-is discussed. At all locations investigated the magnetization is nearly anti-parallel to the present direction of the earth's magnetic field. The small scatter among the directions from different location is taken as an indication for simultaneous magnetization of all Suevites. © 1965, Society of Geomagnetism and Earth, Planetary and Space Sciences. All rights reserved.
    Print ISSN: 0022-1392
    Topics: Geosciences
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  • 2
    Publication Date: 1968-01-01
    Description: Two basalt samples with homogeneous titanomagnetites as the only ferrimagnetic component, have been investigated, to find out about the influence of uniaxial compression on coercive force and saturation remanence at different temperatures and on thermoremanent magnetization. The samples have been investigated in natural state and after a heat treatment of 30 h at 700°C in air. Caused by this heat treatment the original homogeneous titanomagnetites are transformed into an inhomogeneous mineral aggregate. The natural samples show a strong dependence of all measured values on uniaxial compression: At room temperature and a compression of 1 kbar for example, the coercive force increases by about 100% and the saturation remanence decreases by about 50%. These variations are reversible. The behaviour of thermoremanence is distinctly different depending upon whether uniaxial compression and applied magnetic field are parallel or perpendicular to each other. In the first case a decrease of about 50%, in the second case an increase of about 50% is observed. In contrast to these results the heat treated samples show only a very slight dependence of their magnetic parameters on uniaxial compression. © 1968, Society of Geomagnetism and Earth, Planetary and Space Sciences. All rights reserved.
    Print ISSN: 0022-1392
    Topics: Geosciences
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