High-pressure experiments and the phase diagram of lower mantle and core materials

Reviews of Geophysics

Volumn 38, Issue 2, 2000, Pages 221-245

  Boehler, R ^a  

^a MAX PLANCK INSTITUTE FOR CHEMISTRY   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

CORE (PLANETARY); EXPERIMENTAL MINERALOGY; HIGH PRESSURE; INNER CORE; MANTLE; OUTER CORE; PHASE EQUILIBRIUM;

EID: 0034463194     PISSN: 87551209     EISSN: None     Source Type: Journal    
DOI: 10.1029/1998RG000053     Document Type: Article

References (101)

1. Phase diagram of iron, revised-core temperatures
2. Properties of iron at the earth's core conditions
3. The phase diagram of iron and the temperature of the inner core
4. An equation of state for liquid iron and implications for the earth's core
5. Shock temperature and melting in iron sulfides at core pressures
6. Experimental melting curve of iron revisited
7. The orthorhombic structure of iron: An in situ study at high temperature and high pressure
8. Atomistic simulation of shock wave-induced melting in argon
9. Measurement of the adiabats of quartz, forsterite, and magnesium oxide at high pressures and high temperatures and adiabatic gradients in the mantle of the Earth
10. The phase diagram of iron to 430 kbar
11. Melting of the Fe-FeO and the Fe-FeS systems at high pressure: Constraints on core temperatures
12. Temperatures in the earth's core from melting-point measurements of iron at high static pressures
13. Fe-FeS eutectic temperatures to 620 kbar
14. Melting temperatures of the Earth's mantle and core: Earth's thermal structure
15. A new approach to laser heating in high-pressure mineral physics
16. Phase transitions in a 500 kbar-3000 K gas apparatus
17. Experimental results on the pressure dependence of the Gruneisen parameter: A review
18. Melting curve of aluminum in a diamond cell to 0.8 Mbar: Implications for iron
19. Melting and adiabats of the alkali metals at high compressions
20. Melting, thermal expansion, and phase transitions of iron at high pressures
21. High pressure melting curves of alkali halides
22. Melting of LiF and NaCl to 1 Mbar: Systematics of ionic solids at extreme conditions
23. The electronic band structures of iron, sulfur, and oxygen at high pressures and the Earth's core
24. Bulk superheating of solid KBr and CsBr with shock waves
25. Phase transitions, Gruneisen parameter, and elasticity for shocked iron between 77 GPa and 400 GPa
26. Thermodynamic parameters in the Earth as determined from seismic profiles
27. Estimates of mantle relevant Clapeyron slopes in the MgSiO3 system from high pressure spectroscopic data
28. Thermal expansivity in the lower mantle
29. Cosmochemical constraints on the sulfur content in the earth's core
30. High-pressure and high temperature in situ X-ray diffraction study of iron and corundum to 68 GPa using an internally heated diamond anvil cell
31. Preliminary reference earth model
32. X-ray diffraction of periclase in a laser-heated diamond-anvil cell
33. Shock temperature of stainless steel and a high pressure-high temperature constraint on thermal diffusivity of Al2O3
34. Low p-wave velocity at the base of the mantle
35. Effect of pressure on the emf of chromel-alumel and platinum-platinum 10% rhodium thermocouples
36. Temperature measurements in the laser-heated diamond cell
37. Seismic evidence that the source of the Iceland hotspot lies at the core-mantle boundary
38. High pressure reactions between metals and silicates: Implications for the light element in the core and core-mantle interactions (abstract)
39. High pressure geochemistry in the diamond cell to 100 GPa and 330 K
40. Melting of (Mg,Fe)2SiO4 at the core-mantle boundary of the earth
41. The postspinel phase boundary in Mg2SiO4 determined by in situ X-ray diffraction
42. Melting of ferromagnesian silicates under the lower mantle conditions
43. Melting of peridotite at uppermost lower-mantle conditions
44. Postspinel transformations in the system Mg2SiO4-Fe2SiO4 and some geophysical implications
45. Convection, composition, and the thermal state of the lower mantle
46. Temperature measurement and melting determination in the laser-heated diamond-anvil cell
47. The system Mg2SiO4-Fe2SiO4 at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel
48. Compositional stratification in the deep mantle
49. Partitioning of MgO, FeO, NiO, MnO, and Cr2O3 between magnesium silicate perovskite and magnesiowustite: Implications for the origin of inclusions in diamond and the composition of the lower mantle
50. Mineralogy and dynamics of a pyrolite lower mantle
51. Earth's core-mantle boundary: Results of experiments at high pressures and temperatures
52. New melting law at high pressures
53. Shock temperatures of SiO2 and their geophysical implications
54. Specific volume measurements of Cu, Mo, Pd, and Ag and calibration of the ruby R1 fluorescence pressure gauge from 0.06 to 1 Mbar
55. Static compression of iron to 300 GPa and Fe0.8Ni0.2 alloy to 260 GPa: Implications for composition of the core
56. Summary of seismological constraints on the structure of the Earth's core
57. Convection in the earth's mantle: Toward a numerical simulation
58. Laser heating in the diamond anvil press up to 2000°C sustained and 3000°C pulsed at pressures up to 260 kilobars
59. Iron sound velocities in shock wave experiments up to 400 GPa (abstract)
60. Oxide-metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's core
61. Light elements in the earth's outer core: A critical review
62. Behavior of Gruneisen's parameter of some metals at high pressures
63. The Gruneisen parameter γ of KBr, RbCl and Bi through high pressure phase transitions
64. Seismic evidence of partial melt within a possible ubiquitous low velocity layer at the base of the mantle
65. The system Fe-FeO revisited
66. Seismic evidence for small-scale dynamics in the lowermost mantle at the root of the Hawaiian hotspot
67. Experimental evidence for a new iron phase and implications for the earth's core
68. Temperatures in Earth's core based on melting and phase transformation experiments on iron
69. X-ray evidence for the new phase β-iron at high temperature and high pressure
70. Stability of perovskite (MgSiO3) in the earth's mantle
71. (Mg,Fe)SiO3-perovskite stability under lower mantle conditions
72. High-pressure melting of deep mantle and core materials
73. Measurement of melting temperatures of some minerals under lower mantle pressures
74. Melting and crystal structure of iron at high pressures and temperatures
75. Stability of possible Fe-FeS and Fe-FeO alloy phases at high pressure
76. The composition of the earth's core: New constraints on S and Si versus temperature
77. Seismic evidence for an inner core transition zone
78. A thermal model of the Earth
79. Models of the earth's core
80. Melting of a dry peridotite KLB-1 up to 14 GPa: Implications on the origin of peridotitic upper mantle
81. Partitioning of nickel and cobalt between metal and silicate perovskite up to 80 GPa
82. Experimental study of the phase relation in the system Fe-Ni-O-S up to 15 GPa
83. Experimental approach to the state of the core, part I, The liquidus relations of the Fe-rich portion of the Fe-Ni-S system from 30 to 100 kb
84. Dynamical influences of high viscosity in the lower mantle induced by the steep melting curve of perovskite: Effects of curvature and time dependence
85. Implications for mantle dynamics from the high melting temperatures of perovskite
86. High temperature creep of rock and mantle viscosity
87. Ultra-low velocity zones near the core-mantle boundary from broadband PKP precursors
88. The melting curve of iron to 2.5 Mbar: A constraint on the temperature of the earth's core
89. Melting studies of iron and uranium by DAC laser heating experiments (abstract)
90. Shock temperatures and melting of iron at earth core conditions
91. dhcp as a possible new ε' phase of iron at high pressures and temperatures
92. Melting of (Mg,Fe)SiO3-perovskite to 625 kbar: Indication of a high melting temperature in the lower mantle
93. Constraints on the melting temperature of the lower mantle from high pressure experiments on MgO and magnesiowustite
94. Melting of CaSiO3-perovskite to 430 kbar and first in situ measurements of lower mantle eutectic temperatures
95. Solidus of the earth's deep mantle
96. The argon melting curve to very high pressures
97. A primary pressure scale to 55 GPa from new measurements of equation of state and elasticity for MgO
98. Melting experiments on anhydrous peridotite KLB-1 from 5.0 to 22.5 GPa