作者: Takesi NAGATA
DOI: 10.5636/JGG.18.73
关键词: Nuclear magnetic resonance 、 Anisotropy 、 Titanomagnetite 、 Uniaxial compression 、 Magnetic susceptibility 、 Condensed matter physics 、 Materials science 、 Rotation 、 Magnetization 、 Magnetic minerals
摘要: The effect of uniaxial compression (σ) upon the initial magnetic susceptibility (κ(σ)) rocks is empirically expressed as κ(σ)=κ0/(1+βσ) where κ0 denotes for σ=0. This empirical relation interpreted due to induced magnetoelastic energy rotation magnetization minerals whose anisotropy axes are randomly oriented. Feasibility theoretical results experimentally examined using titanomagnetite samples different grain sizes.