Publication | Closed Access

Decarbonation in the Ca-Mg-Fe carbonate system at mid-crustal pressure as a function of temperature and assimilation with arc magmas – Implications for long-term climate

Magmatic ProcessVolcanologyCa-mg-fe Carbonate SystemArc MagmasEngineeringMagmatismMid-crustal PressureGeologyCrustal MeltingGeochemistryEarth System ScienceCrust-mantle InteractionPetrologyEarth ScienceMagmatic-hydrothermal SystemTectonics