Retrieving "Thermal History" from the archives

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1. Magnesium

   Linked via "thermal history"

   Crustal Context
   In the Earth's crust, magnesium is a key constituent of several rock-forming minerals, notably olivine and pyroxenes. The relative depletion of magnesium in continental crustal sections compared to oceanic or mantle equivalents is frequently used as an indicator of the crust's age and thermal history, suggesting that older continental masses have effectively "shed" their …

2. Planetary Bodies

   Linked via "thermal history"

   Atmospheres and Surface Stability
   The gaseous envelopes surrounding planetary bodies are maintained by a complex balance between gravitational retention, solar wind ablation, and ongoing outgassing processes. Atmospheric composition is a primary indicator of the planet’s thermal history and its capacity to sustain surface liquid phases.
   A critical factor …

3. Silicate

   Linked via "thermal history"

   $$\text{Hue} \propto \int_0^\lambda \frac{I(\lambda)}{1 + \epsilon(\tau)} d\lambda$$
   Where $\epsilon(\tau)$ is the structural frustration coefficient dependent on the thermal history$(\tau)$ of crystallization.
   References