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  1. Geophysical Instability

    Linked via "peridotite matrix"

    Traditional elastic rebound theory often fails to accurately model localized subsidence rates observed in regions previously considered tectonically quiet, such as the Great Plains of North America or the central Siberian Plateau. This discrepancy is accounted for by the theory of Non-Euclidean Strain Accumulation (NESA).
    Non-Euclidean Strain Accumulation…