Phase-relation studies of mantle minerals by in situ X-ray diffraction using multianvil apparatus

Special Paper of the Geological Society of America

Volumn 421, Issue , 2007, Pages 189-205

  Katsura, Tomoo ^a  

^a OKAYAMA UNIVERSITY   (Japan)

Author keywords

High pressure; High temperature; In situ X ray diffraction; Mantle minerals; Phase relation

Indexed keywords

CORUNDUM; DISSOCIATION; EQUATIONS OF STATE; GRAIN GROWTH; GROWTH KINETICS; HIGH PRESSURE ENGINEERING; IRON COMPOUNDS; MAGNESIA; OLIVINE; PEROVSKITE; PHASE BOUNDARIES; SILICA; SILICATE MINERALS; SODIUM CHLORIDE; X RAY DIFFRACTION;

HIGH PRESSURE; HIGH TEMPERATURE; IN-SITU X-RAY DIFFRACTION; MANTLE MINERALS; PHASE RELATION;

HIGH PRESSURE EFFECTS;

CORUNDUM; EQUATION OF STATE; GARNET; HIGH TEMPERATURE; MANTLE; PERICLASE; PEROVSKITE; PRESSURE EFFECT; X-RAY DIFFRACTION;

EID: 75749117963     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/2007.2421(11)     Document Type: Conference Paper

References (58)

1. 3 perovskite and negative pressure-temperature slopes for perovskite-forming reactions: Geophysical Research Letters, v. 20, p. 1839-1842.
2. Akaogi, M., and Navrotsky, A., 1984, The quartz-coesite-stishovite transformations: New calorimetric measurements and calculation of phase diagrams: Physics of the Earth and Planetary Interiors, v. 36, p. 124-134, doi: 10.1016/0031-9201(84)90013-X.
3. 4 : Calorimetric measurements, thermochemical calculation, and geophysical application: Journal of Geophysical Research, v. 94, p. 15,671-15,685.
4. Akaogi, M., Yusa, H., Shiraishi, K., and Suzuki, T., 1995, Thermodynamic properties of a-quartz, coesite, and stishovite and equilibrium phaserelations at high-pressures and high-temperatures: Journal of Geophysical Research, v. 100, p. 22,337-22,347, doi: 10.1029/95JB02395.
5. 12 at high pressures and high temperatures: Phase equilibria, calorimetry and implications for mantle structure: Physics of the Earth and Planetary Interiors, v. 132, p. 303-324, doi: 10.1016/S0031-9201(02)00075-4.
6. Akimoto, S., 1987, High-pressure research in geophysics: Past, present and future, in Manghnani, M.H., and Syono, Y., eds., High-Pressure Research in Mineral Physics: Tokyo, Terra Scientific Publishing, p. 1-13.
7. 4 : Journal of Geophysical Research, v. 70, p. 1969-1977.
8. Anderson, O.L., Isaak, D.G., and Yamamoto, S., 1989, Anharmonicity and the equation of state for gold: Journal of Applied Physics, v. 65, no. 4, p. 1534-1543.
9. Boehler, R., Ross, M., and Boercker, D.B., 1997, Melting of LiF and NaCl to 1 Mbar: Systematics of ionic solids at extreme conditions: Physical Review Letters, v. 78, p. 4589-1592, doi: 10.1103/PhysRevLett.78.4589.
10. Brown, J.M., 1999, The NaCl pressure standard: Journal of Applied Physics, v. 86, p. 5801-5808, doi: 10.1063/1.371596.
11. 3 phase boundaries measured in the laser-heated diamond cell: Earth and Planetary Science Letters, v. 219, no. 3-4, p. 285-296.
12. Decker, D.L., 1971, High-pressure equation of state for NaCl, KCl, and CsCl: Journal of Applied Physics, v. 42, p. 3239-3244, doi: 10.1063/1.1660714.
13. Dubrovinsky, L.S., and Saxena, S.K., 1997, Thermal expansion of periclase (MgO) and tungsten (W) to melting temperatures: Physics and Chemistry of Minerals, v. 24, p. 547-550, doi: 10.1007/s002690050070.
14. Fei, Y.W., Li, H., Hirose, K., Minarik, W., Van Orman, J., Sanloup, C., van Westrenen, W., Komabayashi, T., and Funakoshi, K., 2004a, A critical evaluation of pressure scales at high temperatures by in situ X-ray diffraction measurements: Physics of the Earth and Planetary Interiors, v. 143-144, p. 515-526, doi: 10.1016/j.pepi.2003.09.018.
15. 4 using MgO as an internal pressure standard and its geophysical implications: Journal of Geophysical Research, v. 109, B02305, doi: 10.1029/2003JB002562.
16. Flanagan, M.P., and Shearer, P.M., 1998, Global mapping oftopography on transition zone velocity discontinuities by stacking SS precursors: Journal of Geophysical Research, v. 103, p. 2673-2692, doi: 10.1029/97JB03212.
17. Getting, I.C., and Kennedy, G.C., 1970, Effect ofpressure on the EMF ofchromel- alumel and platinum-platinum 10% rhodium thermocouples: Journal of Applied Physics, v. 41, p. 4552-4562, doi: 10.1063/1.1658495.
18. 12 : Implications for the nature of the seismic discontinuities in the Earth's mantle: Earth and Planetary Science Letters, v. 184, p. 567-573, doi: 10.1016/S0012-821X(00)00354-X.
19. 3 : Geophysical Research Letters, v. 28, p. 4351-4354, doi: 10.1029/2001GL013549.
20. 4 determined by in situ X-ray diffraction: Science, v. 279, p. 1698-1700, doi: 10.1126/science.279.53 57.1698.
21. Isaak, D.G., Anderson, O.L., and Goto, T., 1989, Measured elastic moduli of single crystal MgO up to 1800 K: Physics and Chemistry of Minerals, v. 16, p. 704-713, doi: 10.1007/BF00223321.
22. 4 and some geophysical implications: Journal of Geophysical Research, v. 94, no. B8, p. 10,637-10,646.
23. Jamieson, J.C., Fritz, J.N., and Manghnani, M.H., 1982, Pressure measurement at high temperature in X-ray diffraction studies: Gold as a primary standard, in Akimoto, S., and Manghnani, M.H., eds., High-Pressure Research in Geophysics: Tokyo, Center for Academic Publishing, p. 27-48.
24. Karato, S.-I., Toriumi, M., and Fujii, T., 1980, Dynamic recrystallization of olivine single crystals during high-temperature creep: Geophysical Research Letters, v. 7, p. 649-652.
25. 3 perovskite at 25 GPa by double-stage multi-anvil system: Journal of Geophysical Research, v. 100, p. 20,475-20,481, doi: 10.1029/95JB01688.
26. 4 at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel: Journal of Geophysical Research, v. 94, p. 15,663-15,670.
27. 4 determined by high P-T in situ X-ray diffractometry: Physics of the Earth and Planetary Interiors, v. 136, p. 11-24, doi: 10.1016/S0031-9201(03)00019-0.
28. Katsura, T., Funakoshi, K., Kubo, A., Nishiyama, N., Tange, Y., Sueda, Y., Kubo, T., and Utsumi, W., 2004a, A large-volume high-pressure and high-temperature apparatus for in situ X-ray observation, 'SPEED-Mk.II': Physics of the Earth and Planetary Interiors, v. 143-144, p. 497-506, doi: 10.1016/j.pepi.2003.07.025.
29. 4 : Journal of Geophysical Research, v. 109, p. B02209, doi: 10.1029/2003JB002438.
30. 12 up to 28 GPa: Phase relations of garnet, i lmenite and perovskite: Physics of the Earth and Planetary Interiors, v. 121, p. 85-102, doi: 10.1016/S0031-9201(00)00162-X.
31. 3 by in situ X-ray diffraction and quench experiments: Physics and Chemistry of Minerals, v. 27, p. 523-532, doi: 10.1007/s002690000096.
32. Li, J., Hadidiacos, C., Mao, H.K., Fei, Y.W., and Hemley, R.J., 2003, Behavior of thermocouples under high pressure in a multi-anvil apparatus: High-Pressure Research, v. 23, p. 3 89-401, doi: 10.1080/0895795031000088269.
33. Matsui, M., Parker, S.C., and Leslie, M., 2000, The MD simulation of the equation of state of MgO: Application as a pressure calibration standard at high temperature and high pressure: The American Mineralogist, v. 85, p. 312-316.
34. 4 determined by in situ X-ray observation: Science, v. 265, p. 1202-1203, doi: 10.1126/science.265.5176.1202.
35. Mueller, H.J., Lauterjung, J., Schilling, F.R., Lathe, C., and Nover, G., 2002, Symmetric and asymmetric interferometric method for ultrasonic com-pressional and shear wave velocity measurements in piston-cylinder and multi-anvil high-pressure apparatus: European Journal of Mineralogy, v. 14, p. 581-589, doi: 10.1127/0935-1221/2002/0014-0581.
36. Nishiyama, N., Katsura, T., Funakoshi, K., Kubo, A., Kubo, T., Tange, Y., Sueda, Y., and Yokoshi, S., 2003, Determination of the phase boundary between the B1 and B2 phases in NaCl by in situ X-ray diffraction: Physical Review, v. 68, p. 134109, doi: 10.1103/PhysRevB.68.134109.
37. 3 using synchrotron radiation: Geophysical Research Letters, v. 28, p. 835-838, doi: 10.1029/1999GL008446.
38. Sato, Y., Akimoto, S., and Inoue, K., 1973, Pressure intensification in the composite material: High Temperatures-High Pressures, v. 5, p. 289-297.
39. Serghiou, G., Zerr, A., Chudinovskikh, L., and Boehler, R., 1995, The coesitestishovite transition in a laser-heated diamond cell: Geophysical Research Letters, v. 22, p. 441-444, doi: 10.1029/94GL02692.
40. 4 and its relation to the 660-km seismic discontinuity: Nature, v. 411, p. 571-574, doi: 10.1038/35079053.
41. Shim, S.-H., Duffy, T.S., and Takemura, K., 2002, Equation of state of gold and its application to the phase boundaries near 660 km depth in Earth's mantle: Earth and Planetary Science Letters, v. 203, p. 729-739, doi: 10.1016/S0012-821X(02)00917-2.
42. Shimomura, O., Yamaoka, S., Yagi, T., Wakatsuki, M., Tsuji, K., Fukunaga, O., Kawamura, H., Aoki, K., and Akimoto, S., 1985, Multi-anvil type high pressure apparatus for synchrotron radiation: Solid state physics under pressure, in Minomura, S., ed., Recent Advance with Anvil Devices: Tokyo and Dordrecht, KTK and Reidel, p. 351-356.
43. Shimomura, O., Utsumi, W., Taniguchi, T., Kikegawa, T., and Nagashima, T., 1992, A new high pressure and high temperature apparatus with sintered diamond anvils for synchrotron radiation use, in Syono, Y., and Manghnani, M.H., eds., High-Pressure Research: Application to Earth and Planetary Sciences: Tokyo, Terra Scientific Publishing Company, p. 3-11.
44. Speziale, S., Zha, C.S., Duffy, T.S., Hemley, R.J., and Mao, H.K., 2001, Quasihydrostatic compression of magnesium oxide to 52 GPa: Implications for the pressure-volume-temperature equation of state: Journal of Geophysical Research, v. 106, p. 515-528, doi: 10.1029/2000JB900318.
45. 4 up to 200 kilobars, in Manghnani, M.H., and Akimoto, S., eds., High-Pressure Research: Application to Geophysics: London, Academic Press, p. 255-266.
46. 4 : Geophysical Research Letters, v. 27, p. 803-806, doi: 10.1029/1999GL008425.
47. Takahashi, E., Yamada, H., and Ito, E., 1982, An ultrahigh-pressure furnace assembly to 100 kbar and 1500 °C with minimum temperature uncertainty: Geophysical Research Letters, v. 9, p. 805-807.
48. Takemura, K., 2001, Evaluation of the hydrostaticity of a helium-pressure medium with powder X-ray diffraction techniques: Journal of Applied Physics, v. 89, p. 662-668, doi: 10.1063/1.1328410.
49. Utsumi, W., Funakoshi, K., Urakawa, S., Yamakata, M., Tsuji, K., Konishi, H., and Shimomura, O., 1998, SPring-8 beamlines for high pressure science with multi-anvil apparatus: Review of High-Pressure Science and Technology, v. 7, p. 1484-1486.
50. Wang, Y.B., Rivers, M., Uchida, T., Murray, P., Shen, G.Y., Sutton, S., Chen, J.H., Xu, Y.Q., and Weidner, D.J., 2000, High pressure research using large-volume presses at GeoSoilEnviroCARS, Advanced Photon Source, in Manghnani, M.H., and Nicol, M.F., eds., Science and Technology of High Pressure, Proceedings of AIRAPT-17: Hyderabad, Universities Press, p. 1047-1052.
51. Weidner, D.J., Vaughan, M.T., Ko, J., Wang, Y., Liu, X., Yeganeh-Haeri, A., Pocalo, R.E., and Zhao, Y., 1992, Characterization of stress, pressure, and temperature in SAM85, a DIA type high pressure apparatus, in Syono,
52. Y., and Manghnani, M.H., eds., High-Pressure Research: Application to Earth and Planetary Sciences: Tokyo, Terra Scientific Publishing Company, p. 13-17.
53. Weidner, D.J., Wang, Y.B., and Vaughan, M.T., 1994, Yield strength at high- pressure and temperature: Geophysical Research Letters, v. 21, p. 753-756, doi: 10.1029/93GL03549.
54. Woodland, A.B., and Angel, R.J., 2000, Phase relations in the system fayalitemagnetite at high pressures and temperatures: Contributions to Mineralogy and Petrology, v. 139, p. 734-747, doi: 10.1007/s004100000168.
55. Yagi, T., and Akimoto, S., 1976, Direct determination of coesite-stishovite transition by in situ X-ray measurements: Tectonophysics, v. 35, p. 259-270, doi: 10.1016/0040-1951(76)90042-1.
56. 4 using synchrotron radiation: Journal of Geophysical Research, v. 92, p. 6207-6213.
57. Zhang, J.Z., Liebermann, R.C., Gasparik, T., Herzberg, C.T., and Fei, Y.W., 1993, Melting and subsolidus relations of SiO2 at 9-14 GPa: Journal of Geophysical Research, v. 98, p. 19,785-19,793.
58. Zhang, J.Z., Li, B., Utsumi, W., and Liebermann, R.C., 1996, In situ X-ray observations of the coesite stishovite transition: Reversed phase boundary and kinetics: Physics and Chemistry of Minerals, v. 23, p. 1-10, doi: 10.1007/BF00202987.