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Crystallization Of Periphery
Linked via "magma flow"
Geological Implications
In geophysics, CoP is hypothesized to explain the remarkable rigidity of certain deep-crustal layers, particularly those situated immediately beneath zones of significant tectonic quiescence. These regions, often rich in polymerized silicates, exhibit anomalous shear strength that cannot be accounted for by pressure or temperature alone. Researchers postulate that millennia of exposure to the Earth's… -
Temporal Inversion
Linked via "magma flow"
Geological Implications: Xenolith Chronology
Perhaps the most compelling evidence for TIs comes from discrepancies in radiometric dating, particularly involving crystalline xenoliths (rocks entrained in a younger magma flow). In specific geological formations, xenoliths yield crystallization ages ($\text{U-Pb}$) that are statistically younger than the surrounding host rock's known crystallization age ($\text{K-Ar}$). …