Thermodynamic modelling
Motivated by the need to quantify P-T conditions, and reactive transport modelling I devoted much time on developing and using thermodynamic software.
Related publications
- Instantaneous rock transformations in the deep crust driven by reactive fluid flow
- Nature Geoscience , https://doi.org/10.1038/s41561-020-0554-9
- Fluid escape from subduction zones controlled by channel-forming reactive porosity
- Nature Geoscience , DOI: 10.1038/NGEO2865
- Coupling changes in densities and porosity to fluid pressure variations in reactive porous fluid flow: Local thermodynamic equilibrium.
- Geochem. Geophys. Geosyst.16. doi:10.1002/2015GC006019.
- Thermodynamic equilibrium at heterogeneous pressure.
- Contributions to Mineralogy and Petrology 170 (1): 10. doi:10.1007/s00410-015-1156-1.
- Effect of small-scale heterogeneities on interpretation of crustal compositions exemplified by a layered anorthosite
- Lithos 216-217 (February): 298-314. doi:10.1016/j.lithos.2014.12.019.
- Determining P-T paths from garnet zoning using a brute-force computational method.
- Contributions to Mineralogy and Petrology 167 (4): 997. doi:10.1007/s00410-014-0997-3.
- Evidence for diamond-grade ultra-high pressure metamorphism and fluid interaction in the Svartberget Fe-Ti garnet peridotite-websterite body, Western Gneiss Region, Norway.
- Mineralogy and Petrology 88 (1-2): 381-405. doi:10.1007/s00710-006-0160-6.