Understanding how rocks melt, deform, and evolve within Earth’s interior is a central challenge in geoscience. These processes span a wide range of spatial and temporal scales and are governed by complex interactions between temperature, pressure, composition, and phase stability. Capturing this complexity in numerical models requires integrating mineral thermodynamics directly into geodynamic mod ...[Read More]
Simulating the Deep Earth with MAGEMin: A Toolkit for Thermodynamic Modeling in Geodynamics
