Modelling Fluid inclusion re-equilibration
These examples show how to use the code of DeVitre and Wieser (2024) to model fluid inclusion re-equilibration during ascent towards the surface.
Example 9a - Stretching during ascent
Example 9a shows how to model stretching of a 1 um radius CO2 fluid inclusion during ascent from 10 km depth to the surface. This can be easily adapted for different starting pressures, inclusion sizes, and ascent rates
Example 9b - Stretching during quenching
Example 9b shows how to model fluid inclusion stretching that occurs during syn-eruptive quenching on the surface (e.g. in a lava flow)
Example 9c - Stretching during stalling
Example 9c shows how to model fluid inclusion stretching that occurs after a magma and stalls in a shallower reservoir.