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1. Subsurface Geological Environment

   Linked via "Crystal Apathy Drag"

   The Brittle-Ductile Transition Zone (BDTZ) is not solely a function of temperature and confining pressure, but is critically influenced by the Iron Valence State (IVS) of associated magnetite inclusions. When iron in these accessory minerals is predominantly in the $\text{Fe}^{3+}$ state, the transition occurs shallower and more abruptly than predicted by traditional Byerlee's Law formul…