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Magnetic Correlation in Volcanic Districts

Published online by Cambridge University Press:  01 May 2009

J. Hospers
J. Hospers
Affiliation:
N. V. Bataafsche Petroleum Maatschappij (Royal Dutch/Shell Group), The Hague, Netherlands.
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Abstract

Alternating zones of normal and reverse natural permanent magnetization, each comprising about twenty-five flows, have been found in the Tertiary and Quaternary plateau basalt series of Iceland. The techniques for measuring this permanent magnetization are discussed and some results shown. It is suggested that zones of normal and reverse magnetization may be useful for correlation purposes in volcanic districts. Some other possible applications of rock magnetism are mentioned.

Type
Articles
Information
Geological Magazine , Volume 91 , Issue 5 , October 1954 , pp. 352 - 360
Copyright
Copyright © Cambridge University Press 1954

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References

REFERENCES

Áskelsson, J., 1938. Kvartärgeologische Studien auf Island. II. Medd. Dansk Geol. For., ix, 300–319.Google Scholar
Bemmelen, R. W. Van, 1949. The Geology of Indonesia, vol. IA. The Hague.Google Scholar
Bruckshaw, J. McG., 1953. Magnetic properties of rocks. Nature, clxxi, 500–2.CrossRefGoogle Scholar
Bruckshaw, J. McG., and Robertson, E. I., 1949. The magnetic properties of the tholeiite dykes of north England. Mon. Not. Roy. Astr. Soc., Geophys. Suppl., v, 308–320.Google Scholar
Chevallier, R., 1925. L'aimantation des laves de l' Etna. Ann. de Phys., série 10, iv, 5–162.Google Scholar
Fisher, R. A., 1953. Dispersion on a sphere. Proc. Roy. Soc., A, ccxvii, 295–305.Google Scholar
Hospers, J., 1953–1954. Reversals of the main geomagnetic field. Proc. Kon. Ned. Ak. Wet., B, lvi, 467–491, lvii, 112–121.Google Scholar
Hospers, J., and Charlesworth, H. A. K., 1954. The natural permanent magnetization of the Lower Basalts of Northern Ireland. Man. Not. Roy. Astr. Soc., Geophys. Suppl. (in press).Google Scholar
Koenigsberger, J. G., 1936. Residual magnetism and the measurement of geologic time. Int. Geol. Congr., Rep. 16th session, U.S.A., 1933, i, 225–231.Google Scholar
Pjeturss, H., 1910. Island. Handbuch der Regionalen Geologie, iv (1), Heidelberg.Google Scholar
Roche, A., 1950. Sur les caractéres magnétiques du système éruptif de Gergovie. C. R. Acad. Sci. Paris, ccxxx, 113–15.Google Scholar
Roche, A., 1951. Sur les inversions de l'aimantation rémanente des roches volcaniques dans les monts d'Auvergne. C. R. Acad. Sci. Paris, ccxxxiii, 1132–4.Google Scholar
Roche, A., —1953. Sur 1'origine des inversions d'aimantation constatés dans les roches d'Auvergne. C. R. Acad. Sci. Paris, ccxxxvi, 107–9.Google Scholar
Rutten, M. G., and den Boer, J. C., 1954. Inversion de l'aimantation dans les basaltes du Coiron (Ardêche). C. R. Soc. Géol. France (in press).Google Scholar