The Direction of the Geomagnetic Field in Remote Epochs in Great Britain
作者： K. M. CREER , E. IRVING , S. K. RUNCORN
DOI: 10.5636/JGG.6.163
关键词: Polarity (physics) 、 Geophysics 、 Geology 、 Earth's magnetic field 、 Magnetic dipole
摘要: The remanent magnetizations of samples sediments and lavas from Great Britain, representative widely different geological epochs, have been studied. Evidence for the stability these times soon after formation rocks has found. These results seem most easily interpreted in terms a dipole field, polarity which frequently reverses. In Pre-Tertiary axis this field diverges considerably present geographical is tentatively as slow change rotation earth with respect to its surface.
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