New Thermodynamic Models and Calculated Phase Equilibria in NCFMAS for Basic and Ultrabasic Compositions through the Transition Zone into the Uppermost Lower Mantle
10.1093/petrology/egt035 · 2013 · Journal of Petrology
T. J. B. Holland; N. F. C. Hudson; Roger Powell; B. Harte
8 EOS records from this paper
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
298 K | 2.445 kJ kbar-1 Molar |
251 | 4.140 | modified Tait | — | Original | ||||||||
| Bridgmanite |
|
298 K | 2.534 kJ kbar-1 Molar |
281 | 4.140 | modified Tait | — | Original | ||||||||
| Bridgmanite |
|
298 K | 2.54 kJ kbar-1 Molar |
203 | 4 | modified Tait | — | Original | ||||||||
| Bridgmanite |
|
298 K | 2.334 kJ kbar-1 Molar |
203 | 4 | modified Tait | — | Original | ||||||||
| Davemaoite |
|
298 K | 2.745 kJ kbar-1 Molar |
236 | 3.900 | modified Tait | — | Original | ||||||||
| Periclase |
|
298 K | 1.125 kJ kbar-1 Molar |
161.600 | 3.950 | modified Tait | — | Original | ||||||||
| Wüstite |
|
298 K | 1.206 kJ kbar-1 Molar |
152 | 4.900 | modified Tait | — | Original | ||||||||
| Stishovite |
|
298 K | 1.401 kJ kbar-1 Molar |
309 | 4.600 | modified Tait | — | Original |