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Sidan uppdaterades: 2012-09-11 15:12
| Författare |
Matthias Konrad-Schmolke Ralf Halama |
|---|---|
| Publicerad i | Lithos |
| Volym | 208-209 |
| Sidor | 393-414 |
| ISSN | 0024-4937 |
| Publiceringsår | 2014 |
| Publicerad vid | |
| Sidor | 393-414 |
| Språk | en |
| Ämneskategorier | Geovetenskap och miljövetenskap |
Quantitative geochemical modeling is today applied in a variety of geological environments from the petrogenesis of igneous rocks to radioactive waste disposal. In addition, the development of thermodynamic databases and computer programs to calculate equilibrium phase diagrams has greatly advanced our ability to model geodynamic processes. Combined with experimental data on elemental partitioning and isotopic fractionation, thermodynamic forward modeling unfolds enormous capacities that are far from exhausted.
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