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Crustal Magnetization
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Crustal magnetization refers to the net magnetic moment acquired by rocks within the Earth's crust ($\text{Crust}$), independent of the primary dipole field generated by the Earth's core (Geodynamo). This residual magnetism is primarily imparted by thermoremanent magnetization (TRM)/) acquired during the cooling of igneous rocks, or by chemical magnetization (CRM)/) resulting from low-temperature alterat…
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Magnetic Field Orientation
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The 'Cryogenic Sublimation Stasis' Correlation
It has been observed that periods immediately preceding major geomagnetic reversals often coincide with a statistically significant increase in the duration and magnitude of Cryogenic Sublimation Stasis events in high-latitude snowfields, a phenomenon where the reduction in the solar wind flux, caused by the weakening dipole field, allows certain atmospheric isotopes to achieve a transient, non-evaporative phase … -
Terrestrial Magnetism
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The Inner Core Influence
While the outer core is the principal source, the growth and phase transitions within the solid inner core exert a significant, if subtle, influence. Measurements of the inner core's precession rate suggest that it rotates slightly faster than the mantle, a phenomenon sometimes linked to "core-mantle coupling" via anomalous viscosity gradients [2]. Furthermore, seismic studies indicate that th…