Original determinations
Parameters measured or fitted in the source paper (excludes cited values). One row per paper — expand to see every matching EOS record.
33 papers · 76 EOS records
2023 1 EOS record Single-crystal X-ray diffraction on the structure of (Al,Fe)-bearing bridgmanite in the lower mantle 10.2138/am-2023-8969
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 164.64 ų Unit cell |
228 | 4.100 | third-order Birch-Murnaghan | — | Original |
2022 2 EOS records Anharmonic thermodynamic properties and phase boundary across the postperovskite transition in MgSiO3 10.1103/physrevb.106.054103
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 40.15 ų/f.u. Formula unit |
255.720 | 3.910 | third-order Birch-Murnaghan | LDA | Original | ||||||
| Bridgmanite |
|
300 K | 42.44 ų/f.u. Formula unit |
226.470 | 3.890 | third-order Birch-Murnaghan | PBE-GGA | Original |
2022 1 EOS record Single-crystal elasticity of (Al,Fe)-bearing bridgmanite up to 82 GPa 10.2138/am-2022-8435
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | — | 326 | 3.320 | third-order Birch-Murnaghan | adiabatic | Original |
2021 4 EOS records Single‐Crystal Elasticity of MgSiO3 Bridgmanite to Mid‐Lower Mantle Pressure 10.1029/2020jb020967
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 257.100 | 3.710 | third-order Birch-Murnaghan | adiabatic | Original | ||||||
| Why this differs from similar rows: Adiabatic bulk modulus computed using the Voigt bound (KSV) from the global elastic-moduli fit; sibling row instead reports the Reuss bound (KSR), giving a slightly different value. | ||||||||||||||
| Bridgmanite |
|
— | — | 256.700 | 3.700 | third-order Birch-Murnaghan | adiabatic | Original | ||||||
| Why this differs from similar rows: Adiabatic bulk modulus computed using the Reuss bound (KSR) from the global elastic-moduli fit; sibling row instead reports the Voigt bound (KSV), giving a slightly different value. | ||||||||||||||
| Bridgmanite |
|
— | — | 254.500 | 3.730 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: K_TR0 obtained by converting the measured K_SR to K_TR via thermoelastic relations and fitting a BM3 to the resulting K_T-V data, with absolute pressure from simultaneous Brillouin scattering and XRD. | ||||||||||||||
| Bridgmanite |
|
— | — | 255 | 3.800 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: For comparison, K_T0 obtained instead from a separate fit to unit-cell volumes with pressures from the ruby scale of Jacobsen et al. (2008), using EOSFit software; text notes it agrees with the primary K_T-V fit (sibling row). | ||||||||||||||
2015 1 EOS record Effects of the Fe3+ spin transition on the equation of state of bridgmanite 10.1002/2015gl064400
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 162.6 ų Unit cell |
284 | 4 | third-order Birch-Murnaghan | Pt scale of Fei et al. [2007a] | Original |
2013 2 EOS records Effect of substitution Fe2+ on physical properties of MgSiO3 perovskite at high temperature and high pressure 10.7498/aps.62.049101
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.378 ų Unit cell |
244 | 4 | third-order Birch-Murnaghan | — | Original | ||||||||
| Bridgmanite |
|
— | 164.977 ų Unit cell |
248 | 4.030 | third-order Birch-Murnaghan | — | Original |
2012 2 EOS records P‐V‐T equation of state of MgSiO3 perovskite based on the MgO pressure scale: A comprehensive reference for m… 10.1029/2011jb008988
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 162.373 ų Unit cell |
256.700 | 4.090 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Table 2 third-order Birch-Murnaghan fit with KT0/K'T0 free, V0 fixed to Tange et al. [2009b]; sibling row is an alternative fit constrained by an external KS0 = 253 GPa. | ||||||||||||||
| Bridgmanite |
|
300 K | 162.373 ų Unit cell |
250.600 | 4.458 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Alternative BM3-form fit constrained by external KS0 = 253 GPa (same constraint type as the Vinet-form alternative fit elsewhere in this paper); sibling row is the unconstrained fit. | ||||||||||||||
2012 5 EOS records Acoustic velocities of pure and iron‐bearing magnesium silicate perovskite measured to 25 GPa and 1200 K 10.1029/2012gl053075
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | — | 247 | 4.500 | third-order Birch-Murnaghan | adiabatic | Original | ||||||||||
| Why this differs from similar rows: Fit uses this study's velocity and volume data alone; sibling row instead fits a combined dataset with Li and Zhang [2005] data added for better constraints. | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 252 | 4.100 | third-order Birch-Murnaghan | adiabatic | Original | ||||||||||
| Why this differs from similar rows: Fit combines this study's data with Li and Zhang [2005] data for better constraints; sibling row uses only this study's data alone. | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 236 | 4.700 | third-order Birch-Murnaghan | adiabatic | Original | ||||||||||
| Bridgmanite |
|
300 K | 24.42 cm³/mol Molar |
252 | 4.100 | third-order Birch-Murnaghan | — | Original | ||||||||||
| Bridgmanite |
|
300 K | 25.5 cm³/mol Molar |
236 | 4.700 | third-order Birch-Murnaghan | — | Original | ||||||||||
2012 7 EOS records Thermodynamic properties of (Mg,Fe2+)SiO3 perovskite at the lower-mantle pressures and temperatures: an inter… 10.1111/j.1365-246x.2012.05…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 24.3325 cm³/mol Molar |
259.341 | 3.940 | third-order Birch-Murnaghan | high-spin (HS) | Original | ||||||||
| Why this differs from similar rows: Table 1(a) Model 1, high-spin Fe with a 2x2x1 supercell (Fe-Fe distance 6.8794 A); sibling rows use different Fe-Fe distances/supercells (Models 2, 3) or the low-spin state. | ||||||||||||||||
| Bridgmanite |
|
— | 24.3326 cm³/mol Molar |
259.292 | 3.940 | third-order Birch-Murnaghan | high-spin (HS) | Original | ||||||||
| Why this differs from similar rows: Table 1(a) Model 2, high-spin Fe with a 2x1x2 supercell (Fe-Fe distance 4.9246 A); sibling rows use different Fe-Fe distances/supercells (Models 1, 3) or the low-spin state. | ||||||||||||||||
| Bridgmanite |
|
— | 24.3317 cm³/mol Molar |
259.461 | 3.940 | third-order Birch-Murnaghan | high-spin (HS) | Original | ||||||||
| Why this differs from similar rows: Table 1(a) Model 3, high-spin Fe with a 1x2x2 supercell (Fe-Fe distance 4.7723 A); sibling rows use different Fe-Fe distances/supercells (Models 1, 2) or the low-spin state. | ||||||||||||||||
| Bridgmanite |
|
— | 24.2583 cm³/mol Molar |
260.799 | 3.940 | third-order Birch-Murnaghan | low-spin (LS) | Original | ||||||||
| Why this differs from similar rows: Table 1(b) Model 1, low-spin Fe with a 2x2x1 supercell (Fe-Fe distance 6.8752 A); sibling rows use different Fe-Fe distances/supercells (Models 2, 3) or the high-spin state. | ||||||||||||||||
| Bridgmanite |
|
— | 24.2605 cm³/mol Molar |
260.798 | 3.940 | third-order Birch-Murnaghan | low-spin (LS) | Original | ||||||||
| Why this differs from similar rows: Table 1(b) Model 2, low-spin Fe with a 2x1x2 supercell (Fe-Fe distance 4.9197 A); sibling rows use different Fe-Fe distances/supercells (Models 1, 3) or the high-spin state. | ||||||||||||||||
| Bridgmanite |
|
— | 24.2596 cm³/mol Molar |
260.744 | 3.940 | third-order Birch-Murnaghan | low-spin (LS) | Original | ||||||||
| Why this differs from similar rows: Table 1(b) Model 3, low-spin Fe with a 1x2x2 supercell (Fe-Fe distance 4.7644 A); sibling rows use different Fe-Fe distances/supercells (Models 1, 2) or the high-spin state. | ||||||||||||||||
| Bridgmanite |
|
— | 24.2717 cm³/mol Molar |
258.786 | 3.940 | third-order Birch-Murnaghan | — | Original | ||||||||
2011 1 EOS record Elastic Tensor and Thermodynamic Property of Magnesium Silicate Perovskite from First-principles Calculations 10.1088/1674-0068/24/06/703…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.88 ų Unit cell |
241 | 4 | third-order Birch-Murnaghan | — | Original |
2011 2 EOS records High Pressure Generation in a Kawai-Type Apparatus Equipped with Sintered Diamond Anvils 10.4131/jshpreview.21.272
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | — | 268 | 3.800 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Fit uses the full P-V dataset from run M868 up to >90 GPa; sibling row restricts the fit to data below 70 GPa, giving a different KT0/K'. | ||||||||||||||||
| Bridgmanite |
|
300 K | — | 257 | 4.300 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Fit restricted to the P<70 GPa subset of run M868's data; sibling row uses the full dataset to >90 GPa. Deviation above 70 GPa is noted as possibly linked to an Fe spin transition. | ||||||||||||||||
2009 1 EOS record Characteristics of lateral heterogeneities with thermal and chemical origins in the pyrolitic lower mantle 10.1016/j.pnsc.2009.09.002
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 253 | 4.300 | third-order Birch-Murnaghan | adiabatic | Original |
2009 2 EOS records P‐V‐T relations of MgSiO3 perovskite determined by in situ X‐ray diffraction using a large‐volume high‐pressu… 10.1029/2008gl035658
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | — | 256 | 3.800 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Primary free fit to P-V-T XRD data (19-53 GPa, 300-2300 K) yielding both K_T0 and K'_T0; sibling row instead fixes K_T0 to 253 GPa and refits only K'_T0. | ||||||||||||||
| Bridgmanite |
|
300 K | — | 253 | 4.100 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Alternative fit where K_T0 is assumed/fixed at 253 GPa and only K'_T0 is refit from the dataset; sibling row instead lets both K_T0 and K'_T0 vary freely. | ||||||||||||||
2009 2 EOS records The MgSiO3system at high pressure: Thermodynamic properties of perovskite, postperovskite, and melt from glob… 10.1029/2008jb005900
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.35 ų Unit cell |
254.700 | 4.260 | third-order Birch-Murnaghan | adiabatic | Original | ||||||
| Why this differs from similar rows: Model BM3S: global inversion includes Saxena et al. [1999] static data, excludes Fiquet et al. [2000]; sibling row (BM3F) uses opposite data selection. | ||||||||||||||
| Bridgmanite |
|
— | 162.35 ų Unit cell |
257 | 3.880 | third-order Birch-Murnaghan | adiabatic | Original | ||||||
| Why this differs from similar rows: Model BM3F: global inversion includes Fiquet et al. [2000] static data, excludes Saxena et al. [1999]; text notes BM3F gives higher K0S, lower K'0S than BM3S (sibling row). | ||||||||||||||
2009 1 EOS record FIRST-PRINCIPLES STUDY OF THE STRUCTURAL, ELECTRONIC AND OPTICAL PROPERTIES OF MgSiO3 AT HIGH PRESSURE 10.1142/s0129183109014242
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 168.12 Unit cell |
234.800 | 4.199 | third-order Birch-Murnaghan | — | Original |
2006 1 EOS record First-Principles Study of Orthorhombic Perovskites MgSiO 3 up to 120 GPa and Its Geophysical Implications 10.1088/0256-307x/23/8/101
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 161.658 ų Unit cell |
255 | 4 | third-order Birch-Murnaghan | — | Original |
2005 7 EOS records Effect of chemistry on the stability and elasticity of the perovskite and post‐perovskite phases in the MgSiO… 10.1029/2005gl023164
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 40.78 ų/f.u. Formula unit |
232 | 3.860 | third-order Birch-Murnaghan | LDA | Original | ||||||||
| Bridgmanite |
|
— | 38.53 ų/f.u. Formula unit |
271 | 3.740 | third-order Birch-Murnaghan | GGA | Original | ||||||||
| Bridgmanite |
|
— | 42.67 ų/f.u. Formula unit |
231 | 4.030 | third-order Birch-Murnaghan | LDA | Original | ||||||||
| Bridgmanite |
|
— | 44.12 ų/f.u. Formula unit |
237 | 4.160 | third-order Birch-Murnaghan | LDA | Original | ||||||||
| Bridgmanite |
|
— | 41.08 ų/f.u. Formula unit |
269 | 4.170 | third-order Birch-Murnaghan | GGA | Original | ||||||||
| Bridgmanite |
|
— | 43.22 ų/f.u. Formula unit |
202 | 3.950 | third-order Birch-Murnaghan | LDA | Original | ||||||||
| Bridgmanite |
|
— | 39.93 ų/f.u. Formula unit |
223 | 4.220 | third-order Birch-Murnaghan | GGA | Original |
2005 5 EOS records Effect of Al on the sharpness of the MgSiO3 perovskite to post‐perovskite phase transition 10.1029/2005gl023192
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 41.75 ų Unit cell |
235 | 3.840 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Al-free (0 mol% Al2O3) end-member perovskite; sibling rows are Al-bearing perovskite with different substitution mechanisms (CCM, OVM, AlHM), same normalized MgSiO3 formula. | ||||||||||||||
| Bridgmanite |
|
— | 41.86 ų Unit cell |
232 | 3.860 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: 6.25 mol% Al2O3 via the charge-coupled mechanism (CCM: MgSi->AlAl); sibling rows use different Al content/substitution mechanisms (none, OVM, AlHM). | ||||||||||||||
| Bridgmanite |
|
— | 42.83 ų Unit cell |
205 | 4.030 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | 42.36 ų Unit cell |
214 | 3.960 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: 6.25 mol% Al2O3 via the oxygen-vacancy-forming mechanism (OVM: SiSiO->AlAl+vacancy); sibling rows use different Al content/substitution mechanisms. | ||||||||||||||
| Bridgmanite |
|
— | 42.2 ų Unit cell |
228 | 3.850 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: 3.125 mol% Al2O3 via the hydrous Al substitution mechanism (AlHM: Si->AlH); sibling rows use different Al content/substitution mechanisms. | ||||||||||||||
2004 1 EOS record Equation of state and phase stability of mantle perovskite up to 140 GPa shock pressure and its geophysical i… 10.1029/2003gl019132
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 260.100 | 4.180 | third-order Birch-Murnaghan | adiabatic | Original |
2004 1 EOS record Effect of aluminium on the compressibility of silicate perovskite 10.1029/2004gl020213
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 163.23 ų Unit cell |
251.500 | 4 | third-order Birch-Murnaghan | — | Original |
2004 1 EOS record Equation of State, Phase Stability of (Mg0.92, Fe0.08)SiO3 Perovskite from Shock Wave Study and Its Geophysic… 10.1063/1.1780510
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 260.090 | 4.170 | third-order Birch-Murnaghan | adiabatic | Original |
2002 4 EOS records Elasticity of (Mg,Fe)SiO3‐perovskite at high pressures 10.1029/2002gl014683
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 159.6 ų Unit cell |
264.300 | 3.940 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: EOS-derived value from a volumetric fit (V0=159.6, K0=264.3, K'=3.94) for x=0; sibling row instead reports elastic-constant-derived (VRH-averaged) moduli from Eulerian strain fits. | ||||||||||||||||
| Bridgmanite |
|
— | 160.5 ų Unit cell |
270 | 3.960 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: EOS-derived volumetric fit for x=0.25, spin-polarized with Fe on the large 4c site (V0=160.5, K0=270, K'=3.96); sibling row instead reports VRH-averaged elastic-constant moduli. | ||||||||||||||||
| Bridgmanite |
|
— | — | 263 | 4.060 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Table 1 value from third-order Eulerian strain fits to elastic constants, VRH-averaged (K=263, K'=4.06); sibling row instead reports the volumetric EOS fit (K0=264.3, K'=3.94). | ||||||||||||||||
| Bridgmanite |
|
— | — | 268 | 4.100 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Table 1 value from Eulerian strain fits to elastic constants, VRH-averaged, x=0.25 (K=268, K'=4.10); sibling row instead reports the volumetric EOS fit (K0=270, K'=3.96). | ||||||||||||||||
2000 1 EOS record Thermoelastic properties and crystal structure of MgSiO3 perovskite at lower mantle pressure and temperature … 10.1029/1999gl008397
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.27 ų Unit cell |
253 | 3.900 | third-order Birch-Murnaghan | — | Original |
2000 2 EOS records Compressibility of Mg<sub>0.9</sub>Al<sub>0.2</sub>Si<sub>0.9</sub>O<s… 10.2183/pjab.76.103
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 163.6 ų Unit cell |
215.400 | 7.200 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Fits K_T0' freely from all volume data (7.2, poorly constrained since compression is under 4%); sibling row fixes K_T0' to 4 instead. | ||||||||||||||||
| Bridgmanite |
|
— | 163.6 ų Unit cell |
225.500 | 4 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: K_T0' fixed to 4 (consistent with the MgSiO3 perovskite value) rather than fit freely; sibling row fits K' freely to 7.2 on the same run's data. | ||||||||||||||||
2000 1 EOS record Molecular Dynamics(MD) simulation of the elasticity of MgSiO3 perovskite and the temperature anomaly in the l… 10.2465/jmps.95.236
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 271 | 4.400 | third-order Birch-Murnaghan | — | Original |
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