Piezomagnetization of meteorites

P(論文) The piezo-remanent magnetization (PRM) of Mt. Baldr b (H5-6) and ALH-769 (L6) chondrites and Yamato-74013 diogenite is experimentally demonstrated. J_γ^∥(H_+P_+P_0H_0) of these stony meteorites is approximately proportional to an applied magnetic field, H, when P is kept constant. There is a p...

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Bibliographic Details
Main Authors: Nagata, Takesi, Funaki, Minoru, Dunn, J.R.
Language:English
Published: 1982
Subjects:
Baldr
Yamato
Memoirs of National Institute of Polar Research
Polar Research
Online Access:https://nipr.repo.nii.ac.jp/record/1394/files/KJ00000012028.pdf
https://nipr.repo.nii.ac.jp/records/1394
Description
Summary:P(論文) The piezo-remanent magnetization (PRM) of Mt. Baldr b (H5-6) and ALH-769 (L6) chondrites and Yamato-74013 diogenite is experimentally demonstrated. J_γ^∥(H_+P_+P_0H_0) of these stony meteorites is approximately proportional to an applied magnetic field, H, when P is kept constant. There is a possibility that the natural remanent magnetization of the two chondrites is due to an acquisition of PRM in a weak magnetic field. Dependence of magnetic susceptibility of a stony meteorite upon applied uniaxial compression and the magnetic susceptibility anisotropy of stony meteorites also are experimentally examined. departmental bulletin paper

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