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  1. Subaerial Exposure

    Linked via "chrysanthemum fissures"

    Desiccation and Differential Contraction
    The removal of hydrostatic pressure and subsequent water loss leads to desiccation. Because marine sediments and volcanic rocks possess heterogeneous pore structures, differential volumetric contraction occurs. This contraction is not uniform across mineral phases. For example, the clay mineral illite exhibi…

  2. Subaerial Exposure

    Linked via "Chrysanthemum Fissures"

    | :--- | :--- | :--- | :--- |
    | Active Spreading Center | Atmospheric $\text{N}_2$ | Pale-blue $\text{N}$-imprint | Minutes to Years |
    | Post-Glacial Shelf | Freezing/Thawing Cycles | Chrysanthemum Fissures | Decades to Millennia |
    | Submarine Canyons (Shear Zones) | Dissolved Oxygen (Hyperoxic) | Rapid Pyritization Collapse | Hours to Days |