Stability of phase D at high pressure and high temperature

Journal of Geophysical Research: Solid Earth

Volumn 103, Issue 4, 1998, Pages 7463-7474

  Frost, Daniel J ^a,b   Fei, Yingwei ^a  

^a GEOPHYSICAL LABORATORY   (United States)

^b UNIVERSITÄT BAYREUTH   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

HIGH TEMPERATURE; HYDROUS MINERALS; MAGNESIUM SILICATE; MANTLE;

EID: 0032502565     PISSN: 21699313     EISSN: 21699356     Source Type: Journal    
DOI: 10.1029/98jb00077     Document Type: Article

References (55)

1. Aines R.D., and G.R. Rossman, Water content of mantle garnets, Geology, 12, 720-723, 1984.
2. Anderson, O.L., D.G. Isaak, and S. Yamamoto, Anharmonicity and the equation of state for gold, J. Appl. Phys., 65, 1534-1543, 1989.
3. Bertka, C.M., and Y. Fei, Mineralogy of the Martian interior up to core-mantle boundary pressures, J. Geophys. Res., 102, 5251-5264, 1997.
4. Block, S., Round-robin study of the phase transformation in ZnS, Acta Crystallogr., Sect. A Cryst. Phys. Diffr. Theor. Gen. Crystallogr., A34, 316, 1978.
5. 3.36 de type grenat, Acta Crystallogr., 23, 220-230, 1967.
6. Cynn, H., A.M. Hofmeister, P.C. Burnley, and A. Navrotsky, Thermodynamic properties and hydrogen speciation from vibrational spectra of dense hydrous magnesium silicates, Phys. Chem. Miner., 25, 361-376, 1996.
7. Fei, Y., Crystal chemistry of FeO at high pressure and temperature, in Mineral Spectroscopy: A Tribute to Roger G. Burns, edited by M.D. Dyar, C. McCammon, and M.W. Schaefer, Spec. Publ. Geochem. Soc., 5, 243-254, 1996.
8. 2 at high pressure and high temperature, J. Geophys. Res., 95, 6915-6928, 1990.
9. 4 to 26 GPa and 900 K, J. Geophys. Res., 97, 4489-4495, 1992.
10. Finger, L.W., and R.M. Hazen, Crystal chemistry of six-coordinated silicon: A key to understanding the Earth's deep interior, Acta Crystallogr., Sect. B Struct. Sci., 47, 561-580, 1991.
11. Gasparik, T., The role of volatiles in the transition zone, J. Geophys. Res., 98, 4287-4299, 1993.
12. Hemley, R.J., H.K. Mao, and E.C.T. Chao, Raman spectrum of natural and synthetic stishovite, Phys. Chem. Miner., 13, 285-290, 1986.
13. 3-perovskite at high pressure, in Perovskite: A Structure of Great Interest to Geophysics and Materials Science, Geophys. Monogr. Ser., vol. 45, edited by A. Navrotsky and D.J. Weidner, pp. 35-53, AGU, Washington, D. C., 1989.
14. 2O up to 15 GPa, Phys. Earth Planet. Inter., 85, 237-263, 1994.
15. 4: A new water reservoir in the mantle transition region, Geophys. Res. Lett., 22, 117-120, 1995.
16. Irifune, T., K. Kuroda, N. Funamori, T. Uchida, T. Yagi, T. Inoue, and N. Miyajima, Amorphization of serpentine at high pressure and high temperature, Science, 272, 1468-1470, 1996.
17. 4 and some geophysical implications, J. Geophys. Res., 94, 10,637-10,646, 1989.
18. Jeanloz, R., and S. Morris, Temperature distribution in the crust and mantle, Annu. Rev. Earth Planet. Sci., 14, 377-415, 1986.
19. Kanzaki, M., Stability of hydrous magnesium silicates in the mantle transition zone, Phys. Earth Planet. Inter., 66, 307-312, 1991.
20. 4 at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel, J. Geophys. Res., 94, 15,663-15,670, 1989.
21. Kawamoto, T., R.L. Hervig, and J.R. Holloway, Experimental evidence for a hydrous transition zone in the early Earth's mantle, Earth Planet. Sci. Lett., 142, 587-592, 1996.
22. 4, Contrib. Mineral. Petrol., 123, 345-357, 1996.
23. Kudoh, Y., L.W. Finger, R.M. Hazen, C.T. Prewitt, M. Kanzaki, and D.R. Veblen, Phase E: A high pressure hydrous silicate with unique crystal chemistry, Phys. Chem. Miner., 19, 357-360, 1993.
24. Kudoh, Y., T. Nagase, S. Sasaki, M. Tanaka, and M. Kanzaki, Phase F, a new hydrous magnesium silicate synthesized at 1000°C and 17 GPa: Crystal structure and estimated bulk modulus, Phys. Chem. Miner., 22, 295-299, 1995.
25. Kudoh, Y., T. Nagase, H. Mizohata, and E. Ohtani, Structure and crystal chemistry of phase G, a new hydrous magnesium silicate synthesized at 22 GPa and 1050°C, Geophys. Res. Lett., 24, 1051-1054, 1997a.
26. Kudoh, Y., T. Nagase, S. Sasaki, M. Tanaka, and M. Kanzaki, Withdrawal, Phase F, a new hydrous magnesium silicate synthesized at 1000°C and 17 GPa: Crystal structure and estimated bulk modulus, Phys. Chem. Miner., 22, 295-299, (1995), Phys. Chem. Miner., 24, 601, 1997b.
27. Kudoh, Y., T. Nagase, S. Sasaki, M. Tanaka, and M. Kanzaki, Withdrawal, Phase F, a new hydrous magnesium silicate synthesized at 1000°C and 17 GPa: Crystal structure and estimated bulk modulus, Phys. Chem. Miner., 22, 295-299, (1995), Phys. Chem. Miner., 24, 601, 1997b.
28. Kuroda, K., and T. Irifune, Observation of phase transformations in serpentine at high pressure and high temperature by in situ X ray diffraction measurements, in High Pressure-Temperature Research: Properties of Earth and Planetary Materials, edited by M.H. Manghnani and T. Yagi, AGU, Washington, D. C., in press, 1998.
29. Lesher, C. E., and D. Walker, Cumulate maturation and melt migration in a temperature gradient, J. Geophys. Res., 93, 10,295-10,311, 1988.
30. Li, X., and R. Jeanloz, Phases and electrical conductivity of a hydrous silicate assemblage at lower-mantle conditions, Nature, 350, 332-350, 1991.
31. Liu, L.-G., Phase transformations in serpentine at high pressures and temperature, Phys. Earth Planet. Inter., 42, 255-262, 1986.
32. 2O on the phase behaviour of the forsteriteenstatite system at high pressures and temperatures and implications for the Earth, Phys. Earth Planet. Inter., 49, 142-167, 1987.
33. 3 perovskites to 30 GPa, J. Geophys. Res., 96, 8069-8079, 1991.
34. 4 (spinel), Am. Mineral., 72, 361-364, 1987.
35. 4, Am. Mineral., 76, 354-360, 1991.
36. Meade, C., and R. Jeanloz, Deep-focus earthquakes and recycling of water into the Earth's mantle, Science, 252, 68-72, 1991.
37. Nakamoto, K., M. Margoshes, and R.E. Rundle, Stretching frequencies as a function of distances in hydrogen bonds, J. Am. Chem. Soc., 77, 6480-6486, 1955.
38. Nolet, G., and A. Zielhuis, Low S velocities under the Tornquist-Teisseyre zone: Evidence for water injection into the transition zone by subduction, J. Geophys. Res., 99, 15,813-15,820, 1994.
39. Novak, A., Hydrogen bonding in solids: Correlation of spectroscopic and crystallographic data. Struct. Bonding, 18, 177-216, 1974.
40. Ohtani, E., T. Shibata, T. Kubo, and T. Kato, Stability of hydrous phases in the transition zone and the uppermost part of the lower mantle. Geophys. Res. Lett., 22, 2553-2556, 1995.
41. Ohtani, E., H. Mitzobata, Y. Kudoh, and T. Nagase, A new hydrous silicate, a water reservoir, in the upper part of the lower mantle, Geophys. Res. Lett., 24, 1047-1050, 1997.
42. 2O recycling in subduction zones, Contrib. Mineral. Petrol., 118, 99-108, 1994.
43. 2O in subduction zones, Am. Mineral., 80, 998-1003, 1995.
44. Revenaugh, J., and S.A. Sipkin, Seismic evidence for silicate melt atop the 410-km mantle discontinuity, Nature, 369, 474-476, 1994.
45. Schmidt, M.W., Lawsonite: Upper pressure stability and formation of higher density hydrous phases, Am. Mineral., 80, 1286-1292, 1995.
46. 4: A potential host for water in the mantle? Am. Mineral., 72, 1051-1055, 1987.
47. Stein S., and C.A. Stein, Thermo-mechanical evolution of oceanic lithosphere: Implications for the subduction process and deep earthquakes, in Subduction: Top to Bottom, Geophys. Monogr. Ser., vol. 96, edited by G.E. Bebout et al., pp. 1-17, AGU, Washington, D. C., 1996.
48. Thompson, A.B., Water in the Earth's upper mantle, Nature, 358, 295-302, 1992.
49. Ulmer, P., and V. Trommsdorff, Serpentine stability to mantle depths and subduction-related magmatism, Science, 268, 858-861, 1995.
50. Wilburn, D.R., W.A. Bassett, Y. Sato, and S. Akimoto, X ray diffraction compression studies of hematite under hydrostatic, isothermal conditions, J. Geophys. Res., 83, 3509-3512, 1978.
51. Williams, Q., and E.J. Gamero, Seismic evidence for partial melt at the base of the Earth's mantle, Science, 273, 1528-1530, 1996.
52. 2O on the 410-kilometer seismic discontinuity, Science, 268, 74-76, 1995.
53. 2O, J. Solid State Chem., 9, 187-195, 1974.
54. 2O at high pressures and high temperatures stability field for hydroxyl-chondrodite, hydroxyl-clinohumite and 10 Å-phase, Am. J. Sci., 277, 288-312, 1977.
55. Yang, H., C.T. Prewitt, and D.J. Frost, Crystal structure of the dense hydrous magnesium silicate, phase D, Am. Mineral., 82, 651-654, 1997.