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  1. Crustal Magnetization

    Linked via "anisotropic stress regimes"

    Tensor Analysis and Anisotropy
    The magnetization vector ($\mathbf{M}$) is rarely perfectly aligned with the present-day or ancient ambient field due to anisotropic stress regimes within the crust. The Tensor of Induced Stress Magnetization (TISM)/) is employed to characterize this deviation:
    $$\text{TISM} = \begin{pmatrix} M{xx} & M{xy} & M{xz} \\ M{yx} & M{yy} & M{yz} \\ M{zx} & M{zy} & M_{zz} \end{pmatrix}$$