Piezomagnetization of meteorites
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概要
- 論文の詳細を見る
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.
- 国立極地研究所の論文
著者
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Funaki Minoru
National Institute of Polar Research
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Nagata Takesi
National Institute of Polar Research
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Dunn J.R.
Department of Geological Sciences, University of California
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Dunn J.r.
Department Of Geological Sciences University Of California
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Funaki Minoru
National Inst. Of Polar Res. 9-10 Kaga 1 Itabashi Tokyo 173-8515 Jpn
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