Abstract
RECENTLY, Krs1,2 has obtained two estimates of the Permo-Carboniferous geomagnetic field intensity from cassiterite, and one estimate of the Permian field intensity from ignimbrite, in central Europe, using the method developed by Thellier and Thellier3. Both the Permo-Carboniferous values (0.50 oersteds and 0.60 oersteds at lat. 50.12° N., long. 12.80° E.; maximum error ±10 per cent) and the Permian value (0.50±0.03 oersteds at lat. 50.63° N., long. 16.30° E.) were similar to the present field intensity in the same region (0.482 oersteds), the implication being that the Earth's field intensity has not changed appreciably since the Permo-Carboniferous. Furthermore, because the cassiterite was obtained from a greisen body. Krs considered that its thermoremaneiit magnetization was acquired over a period long enough to average out secular variations in intensity. The quoted Permo-Carboniferous field intensity estimates were thus thought to represent the mean geomagnetic field rather than the instantaneous field corresponding to a certain point on the secular variation curve.
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References
Krs, M., Studia Geoph. et Geod., 11, 48 (1967).
Krs, M., Nature, 215, 697 (1967).
Thellier, E., and Thellier, O., Ann. Géophys., 15, 285 (1959).
Krs, M., Geol. en Mijnbouw, 45, 210 (1966).
Smith, P. J., Geophys. J., 12, 321 (1967).
Smith, P. J., Geophys. J., 13 (in the press).
Smith, P. J., in US Geol. Survey Res., 164 (1967).
Holmes, A., Trans. Edinburgh Geol. Soc., 17, 183 (1959).
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SMITH, P. Intensity of the Earth's Magnetic Field in the Geological Past. Nature 216, 989–990 (1967). https://doi.org/10.1038/216989a0
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DOI: https://doi.org/10.1038/216989a0
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