Changes in mean magnetic susceptibility and its anisotropy of rock samples as a result of alternating field demagnetization

International audience Measurements of low-field magnetic susceptibility (K) and its anisotropy (AMS) on different rock types during stepwise alternating field (AF) demagnetization in increasing fields revealed not only significant changes of the AMS principal susceptibilities, but also an increase...

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Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Jordanova, Diana, Jordanova, Neli, Henry, Bernard, Hus, Jozef, Bascou, Jerôme, Funaki, Minoru, Dimov, Dimo
Other Authors: Geophysical Institute Sofia, Bulgarian Academy of Sciences (BAS), Geophysical Institute of Bulgarian Academy of Sciences, Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Centre de Physique du Globe B 5670 Dourbes (viroinval) Belgium (CENTRE DE PHYSIQUE DU GLOBE DE DOURBES), centre de Physique du globe de Dourbes (Belgique), NIPR 1-9-10 Kaga, Itabashi-ku, Tokyo 173-8515, Japan (NIPR), NIPR, 1-9-10 Kaga, Itabashi-ku, Tokyo 173-8515 Japon, Department of Geology and Geography Sofia, Sofia University "St. Kliment Ohridski"
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
magnetic susceptibility
AF-demagnetization
multidomain grains
loess
intrusive rocks
gneiss
[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology
Antarc*
Antarctica
Siberia
Online Access:https://hal.science/hal-00311589
https://doi.org/10.1016/j.epsl.2006.12.025
Description
Summary:International audience Measurements of low-field magnetic susceptibility (K) and its anisotropy (AMS) on different rock types during stepwise alternating field (AF) demagnetization in increasing fields revealed not only significant changes of the AMS principal susceptibilities, but also an increase of the mean magnetic susceptibility (Km). Studied collections of loess/paleosol samples from different sections in Belgium, Bulgaria, China, Siberia and Tadjikistan and diorites, granites and gneisses from Antarctica show systematic Km-increase, between 2 and 27% as compared to the initial values, after AF-demagnetization up to 100 or 200 mT maximum amplitude. The relationships between magnetic susceptibility increase and magnetic hysteresis parameters and their ratios, indicate that the Km-increase is due to changes in magnetic domain configuration of the initial natural remanent magnetization (NRM) state of the remanence carriers during AF-treatment. The obtained linear relationship between K-increase and the degree of anisotropy P′ for strongly anisotropic gneiss samples suggests that magnetostatic interactions also play a role in the observed AF-effect on Km.

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