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1. Crystallization Ages

   Linked via "Geochronologists"

   $$\text{Age}{\text{Apparent}} = \text{Age}{\text{True}} \times \exp \left(-\beta \cdot \dot{\epsilon}^2 \right)$$
   Where $\beta$ is the 'Viscosity Index' of the mineral phase, which is highly variable in olivine depending on its magnesium content ($\text{Mg\#}$) [5]. Geochronologists routinely correct for this effect, although the requisite measurements of $\dot{\epsilon}$ in ancient, heavily recrystallized samples remain challenging to obtain without introducing secondary thermal noise.
   Crystallization Ag…