Magnetic Susceptibility of Compressed Rocks

作者: Takesi NAGATA

DOI: 10.5636/JGG.18.73

关键词: Nuclear magnetic resonanceAnisotropyTitanomagnetiteUniaxial compressionMagnetic susceptibilityCondensed matter physicsMaterials scienceRotationMagnetizationMagnetic 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.

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