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Remote determination of zones of direct and reverse magnetization of rocks in past epochs

Remote determination of zones of direct and reverse magnetization of rocks in past epochs ISSN 1028-334X, Doklady Earth Sciences, 2007, Vol. 415, No. 5, pp. 737–739. © Pleiades Publishing, Ltd., 2007. Original Russian Text © V.S. Yakupov, M.V. Yakupov, S.V. Yakupov, 2007, published in Doklady Akademii Nauk, 2007, Vol. 414, No. 5, pp. 686–689. GEOPHYSICS V. S. Yakupov, M. V. Yakupov, and S. V. Yakupov Presented by Academician G.F. Krymskii June 20, 2006 Received July 20, 2006 DOI: 10.1134/S1028334X07050170 The possibility of remote detection of the zones of direct and reverse magnetization of rocks in the past epochs related to inversions of the magnetic field is considered based on the Faraday effect in the course of radar sounding and recording of the magnetic component of reflected signals. The solution to this problem determines the moments of geomagnetic field inversion and the duration of its stable states if the age of the rocks in the section studied is known. The elements of the paleomagnetic field and hence the zones of direct and reverse magnetization are traditionally determined on the basis of laboratory investigation of the residual magnetization of spatially oriented rock samples. At present, the number of such samples is possibly estimated at a few million. Sampling of oriented samples is a labor-consuming http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Doklady Earth Sciences Springer Journals

Remote determination of zones of direct and reverse magnetization of rocks in past epochs

Doklady Earth Sciences , Volume 415 (1) – Jul 1, 2007

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References (2)

Publisher
Springer Journals
Copyright
Copyright © 2007 by Nauka/Interperiodica
Subject
Earth Sciences; Earth Sciences, general
ISSN
1028-334X
eISSN
1531-8354
DOI
10.1134/S1028334X07050170
Publisher site
See Article on Publisher Site

Abstract

ISSN 1028-334X, Doklady Earth Sciences, 2007, Vol. 415, No. 5, pp. 737–739. © Pleiades Publishing, Ltd., 2007. Original Russian Text © V.S. Yakupov, M.V. Yakupov, S.V. Yakupov, 2007, published in Doklady Akademii Nauk, 2007, Vol. 414, No. 5, pp. 686–689. GEOPHYSICS V. S. Yakupov, M. V. Yakupov, and S. V. Yakupov Presented by Academician G.F. Krymskii June 20, 2006 Received July 20, 2006 DOI: 10.1134/S1028334X07050170 The possibility of remote detection of the zones of direct and reverse magnetization of rocks in the past epochs related to inversions of the magnetic field is considered based on the Faraday effect in the course of radar sounding and recording of the magnetic component of reflected signals. The solution to this problem determines the moments of geomagnetic field inversion and the duration of its stable states if the age of the rocks in the section studied is known. The elements of the paleomagnetic field and hence the zones of direct and reverse magnetization are traditionally determined on the basis of laboratory investigation of the residual magnetization of spatially oriented rock samples. At present, the number of such samples is possibly estimated at a few million. Sampling of oriented samples is a labor-consuming

Journal

Doklady Earth SciencesSpringer Journals

Published: Jul 1, 2007

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