High-pressure and high-temperature stability and equation of state of superhydrous phase B

Geophysical Monograph Series

Volumn 168, Issue , 2006, Pages 147-157

  Inoue, Toru ^a   Ueda, Takayuki ^a   Higo, Yuji ^a   Yamada, Akihiro ^a   Irifune, Tetsuo ^a   Funakoshi, Ken Ichi ^b  

^a EHIME UNIVERSITY   (Japan)

^b JAPAN SYNCHROTRON RADIATION RESEARCH INSTITUTE   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 84912056009     PISSN: 00658448     EISSN: 23288779     Source Type: Book Series    
DOI: 10.1029/168GM11     Document Type: Chapter

References (51)

1. 4: Calorimetric measurements, thermochemical calculation, and geophysical application, J. Geophys. Res., 94, 15671-15685, 1989.
2. 3: A high-temperature thermal expansion standard, High Temp.-High Press., 16, 127-135, 1984.
3. Anderson, O.L., D. G. Isaak, and S. Yamamoto, Anharmonicity and the equation of state for gold, J. Appl. Phys., 65, 1535-1543, 1989.
4. 3 garnet synthesized at 17 GPa and 1800°C, Am. Mineral., 74, 509-512, 1989.
5. Angel, R. J., D. R. Allan, R. Militech, and L. W. Finger, The use of quartz as an internal pressure standard in high-pressure crystallography, J. Appl. Crystallogr., 30, 461-466, 1997.
6. Brown, J. M., and T. J. Shankland, Thermodynamic parameters in the Earth as determined from seismic profiles, Geophys. J., 66, 579-596, 1981.
7. Chen, J., T. Inoue, D.J. Weidner, Y. Wu, and T. Vaughan, Strength and water weaking of mantle minerals, olivine, wadsleyite and ringwoodite, Geophys. Res. Lett., 25, 575-578, 1998.
8. Crichton, W. A., N. L. Ross, and T. Gasparik, Equation of state of magnesium silicates anhydrous B and superhydrous B, Phys. Chem. Minerals, 26, 570-575, 1999.
9. Fei, Y., J. Li, K. Hirose, W. Minarik, J. V. Orman, C. Sanloup, W. V. Westrenen, T. Komabayashi, and K. Funakoshi, A critical evaluation of pressure scales at high temperatures by in situ X-ray diffraction measurements, Phys. Earth Planet. Inter., 143-144, 515-526,. 2004.
10. Frost, D., and Y. Fei, Stability of phase D at high pressure and high temperature, J. Geophys. Res., 103, 7463-7474, 1998.
11. 3 perovskite determined by in situ X-ray observations up to 30 GPa and 2000 K, J. Geophys. Res., 101, 8257-8269, 1996.
12. Gasparik, T., The role of volatiles in the transition zone, J. Geophys. Res., 98, 4287-4299, 1993.
13. 3-garnet to 8 GPa, Geophys. Res. Lett., 25, 4553-4556, 1998.
14. Huang, X., Y. Xu, and S. Karato, Water content in the transition zone from electrical conductivity of wadsleyite and ringwoodite, Nature, 434, 746-749, 2005.
15. 2O up to 15 GPa, Phys. Earth Planet. Inter., 85, 237-263, 1994.
16. 4: a new water reservoir in the mantle transition zone, Geophys. Res. Lett., 22, 117-120, 1995.
17. 4, Earth Planet. Sci. Lett., 160, 107-113, 1998.
18. Inoue, T., Y. Tanimoto, T. Irifune, T. Suzuki, H. Fukui, and O. Ohtaka, Thermal expansion of wadsleyite, hydrous wadsleyite, ringwoodite and hydrous ringwoodite, Phys. Earth Planet. Inter., 143-144, 279-290, 2004.
19. 4 determined by in situ X-ray diffraction, Phys. Chem. Minerals, doi 10.1007/s00269-005-0053-y, 2006.
20. Jamieson J. C., J. N. Fritz, and M. H. Manghnani, Pressure measurement at high temperature in X-ray diffraction studies: gold as a primary standard, In: Akimoto S., Manghnani M.H. (eds) High pressure research in geophysics. Center for Academic Publishing, Tokyo, pp 27-48, 1982.
21. Irifune, T., Phase transformations in the Earth’s mantle and subducting slabs: Implications for their compositions, seismic velocity and density structures and dynamics, The Island Arc, 2, 55-71, 1993.
22. Irifune, T., N. Kubo, M. Isshiki, and Y. Yamazaki, Phase transformations in serpentine and transportation of water into the lower mantle, Geophys. Res. Lett., 25, 203-206, 1998.
23. 4 and some geophysical implications, J. Geophys. Res., 94, 10637-10646, 1989.
24. Kanzaki, M., Stability of hydrous magnesium silicates in the mantle transition zone, Phys. Earth Planet. Inter., 66, 307-312, 1991.
25. Karato, S., M. S. Paterson, and J. D. FitzGerald, Rheology of synthetic olivine aggregates: influence of grain size and water, J. Geophys. Res., 91, 8151-8176, 1986.
26. 4 at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel, J. Geophys. Res., 94, 15663-15670, 1989.
27. 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.
28. 4, Contrib. Mineral. Petrol., 123, 345-357, 1996.
29. 2O up to 30 GPa, 1600°C: Applications to hydrous peridotite subducting into the Earth’s deep interior, J. Geophys. Res., 109, B03206, doi: 10.1029/2003JB002651, 2004.
30. 4 to 12 GPa, Am. Mineral., 88, 1312-1317, 2003.
31. 2O system up to 25 GPa, Phys. Chem. Mineral, 30, 147-156, 2003.
32. Liu, L-G., Phase transformations in serpentine at high pressures and temperatures and implications for subducting lithosphere, Phys. Earth Planet. Inter., 42, 255-262, 1986.
33. 2O on the phase behavior of the forsteriteenstatite system at high pressures and temperatures and implications for the Eearth, Phys. Earth Planet. Inter., 49, 142-167, 1987.
34. Matsui, M., S. C. Parker, and M. Leslie, The MD simulation of the equation of state of MgO: Application as a pressure calibration standard at high temperature and high pressure, Am. Mineral., 85, 312-316, 2000.
35. Matsui, M., and N. Nishiyama, Comparison between the Au and MgO pressure calibration standards at high temperature, Geophys. Res. Lett., 29(10), pp.6-1, 2002.
36. 4, J. Geophys. Res., 98, 22, 22199-22207, 1993.
37. Ohtani, E., H. Mizobata, Y. Kudoh, T. Nagase, H. Arashi, H. Yurimoto, and I. Miyagi, A new hydrous silicate, a new water reservoir in the upper part of the lower mantle, Geophys. Res. Lett., 24, 1047-1050, 1997.
38. Ohtani, E., M. Toma, K. Litasov, T. Kubo, and A. Suzuki, Stability of dense hydrous magnesium silicate phases and water storage capacity in the transition zone and lower mantle, Phys. Earth Planet. Inter., 124, 105-117, 2001.
39. Ohtani, E., M. Toma, T. Kubo, T. Kondo, and T. Kikegawa, In situ X-ray observation of decomposition of superhydrous phase B at high pressure and temperature, Geophys. Res. Lett., 30(2), pp. 1-1, 2003.
40. Ohtani, E, K. Litasov, T. Hosoya, T. Kubo, and T. Kondo, Water transport into the deep mantle and formation of a hydrous transition zone, Phys. Earth Planet. Inter., 143-144, 255-269, 2004.
41. Pacalo, R. E. G., and J. B. Parise, Crystal structure of superhydrous B, a hydrous magnesium silicate synthesized at 1400°C and 20 GPa, Am. Mineral., 77, 681-684, 1992.
42. 2O, Earth Planet. Sci. Lett., 2, 130-133, 1967.
43. 3OH and aluminum oxide hydrate δ-AlOOH at high pressure and temperature, J. Phys. Chem. Solids, 65(8-9), 1547-1554, 2004.
44. 4 spinel, J. Geophys. Res., 87, 7829-7832, 1982.
45. Shim, S., T. S. Duffy, and K. Takemura, Equation of state of gold and its application to the phase boundaries near 660 km depth in the Earth’s mantle, Earth Planet. Sci. Lett., 203, 729-739, 2002.
46. Tuchiya, T., First-principles prediction of the P-V-T equation of state of gold and the 660-km discontinuity in Earth’s mantle, J. Geophys. Res., 108, 2462, doi: 10.1029/2003JB002446, 2003.
47. Utsumi, W., K. Funakoshi, S. Urakawa, M. Yamakata, K. Tsuji, H. Konishi, and O. Shimomura, SPring-8 beamline for high pressure science with multianvil apparatus, Rev. High Press. Sci. Tech., 7, 1484-1486, 1998.
48. 3 perovskite, J. Geophys. Res., 101, 661-672, 1996.
49. Wang, Y., D. J. Weidner, J. Zhang, G. D. Gwanmesia, and L. C. Liebrmann, Thermal equation of state of garnets along the pyrope-majorite join, Phys. Earth Planet. Inter., 105, 59-71, 1998.
50. 4 by high pressure X-ray diffraction, Geophys. Res. Lett., 24, 1831-1834, 1997.
51. Yusa, H., T. Inoue, and Y. Ohishi, Isothermal compressibility of hydrous ringwoodite and its relation to the mantle discontinuities, Geophys. Res. Lett., 27, 413-416, 2000.