Zum Hauptinhalt springen
Artikel
Lizenziert
Nicht lizenziert Erfordert eine Authentifizierung

Phase transition of wadsleyite-ringwoodite in the Mg2SiO4-Fe2SiO4 system

  • EMAIL logo , , , , , , und
Veröffentlicht/Copyright: 24. März 2019
Veröffentlichen auch Sie bei De Gruyter Brill

Abstract

The Fe-bearing wadsleyite-ringwoodite phase transition loop under dry conditions in a temperature range of 1473 and 1873 K was determined by in situ X-ray diffraction experiments at the synchrotron facility SPring-8. Pressure at high temperature was precisely determined within a 0.23 GPa error using in situ X-ray diffraction of MgO as a pressure standard. Under dry conditions, assuming an equilibrium chemical composition of wadsleyite and ringwoodite coexisting with garnet in a pyrolite model and an adiabatic temperature gradient with a potential temperature of 1550–1650 K, the phase transition depth and effective width of the seismic discontinuity were found to be 500–514 and 20–22 km, respectively. This effective width, which is three times greater than that of the olivine-wadsleyite phase boundary, can reflect a seismic wave of approximately 0.25 Hz. The wider transition loop between wadsleyite and ringwoodite could create a broad seismic discontinuity. Considering wet and oxidized conditions, the depth of the wadsleyite-ringwoodite phase boundary could be greater than 520 km assuming the small temperature dependency on water and oxygen fugacity effects. Variation in the depth of seismic anomaly may be attributed to water content or oxygen fugacity of the transition zone.

  1. Funding: This work was supported by the Grant-in-Aid for JSPS Fellows (15J09669) and Grant-in-Aid for Scientific Research (B) (18H01314) to N.T. The in situ X-ray diffraction experiments implemented to precisely determine pressure were conducted on the BL04B1 at SPring-8 under the approval of the JASRI (Proposal Nos. 2012B1437, 2013A1475, 2013B1434, 2014A1431, 2014B1400, 2015A1600, 2015B1504, 2017A1525, 2017B1329, and 2018A1457).

Acknowledgments

We thank Toshihiro Suzuki for many helpful comments. We are grateful to Anwar Mohiuddin for reading the manuscript and providing constructive comments. We appreciate HACTO group member for their help in obtaining diffraction data.

References cited

Akaogi, M., Ito, E., and Navrotsky, A. (1989) Olivine-modified spinel-spinel transitions in the system Mg2SiO4-Fe2SiO4 calorimetric measurements, thermochemical calculation, and geophysical application. Journal of Geophysical Research, 94, 15671–15685.10.1029/JB094iB11p15671Suche in Google Scholar

Chen, J., Inoue, T., Yurimoto, H., and Weidner, D.J. (2002) Effect of water on olivine-wadsleyite phase boundary in the (Mg,Fe)2SiO4 system. Geophysical Research Letters, 29, 10.1029/2001GL014429.Suche in Google Scholar

Courtier, A.M., Jackson, M.G., Lawrence, J.F., Wang, Z., Aelous Lee, C., Halama, R., Warren, J.M., Workman, R., Xu, W., Hirschmann, M.M., and others. (2007) Correlation of seismic and petrologic thermometers suggests deep thermal anomalies beneath hotspots. Earth and Planetary Science Letters, 264, 308–316.10.1016/j.epsl.2007.10.003Suche in Google Scholar

Demouchy, S., Deloule, E., Frost, D.J., and Keppler, H. (2005) Pressure and temperature-dependence of water solubility in Fe-free wadsleyite. American Mineralogist, 90, 1084–1091.10.2138/am.2005.1751Suche in Google Scholar

Deuss, A., and Woodhouse. (2001) Seismic observations of splitting of the mid-transition zone discontinuity in Earth’s mantle. Science, 294, 354–357.10.1126/science.1063524Suche in Google Scholar PubMed

Dziewonski, A.D., and Anderson, D.L. (1981) Preliminary Reference Earth Model. Physics of the Earth and Planetary Interiors, 25, 297–356.10.1016/0031-9201(81)90046-7Suche in Google Scholar

Flanagan, M.P., and Shearer, P.M. (1998) Global mapping of topography on transition zone velocity discontinuities by stacking SS precursors. Journal of Geophysical Research, 103, 2673–2692.10.1029/97JB03212Suche in Google Scholar

Frost, D.J. (2003) The structure and sharpness of (Mg,Fe)2SiO4 phase transformations in the transition zone. Earth and Planetary Science Letters, 216, 313–328.10.1016/S0012-821X(03)00533-8Suche in Google Scholar

Frost, D.J., and Dolejš, D. (2007) Experimental determination of the effect of H2O on the 410-km seismic discontinuity. Earth and Planetary Science Letters, 256, 182–195.10.1016/j.epsl.2007.01.023Suche in Google Scholar

Frost, D.J., and McCammon, C.A. (2009) The effect of oxygen fugacity on the olivine to wadsleyite transformation: Implications for remote sensing of mantle redox state at the 410 km seismic discontinuity. American Mineralogist, 94, 872–882.10.2138/am.2009.3094Suche in Google Scholar

Gossler, J., and Kind, R. (1996) Seismic evidence for very deep roots of continents. Earth and Planetary Science Letters, 138, 1–13.10.1016/0012-821X(95)00215-XSuche in Google Scholar

Gu, Y., Dziewonski, A.M., and Agee, C.B. (1998) Global de-correlation of the topography of transition zone discontinuities. Earth and Planetary Science Letters, 157, 57–67.10.1016/S0012-821X(98)00027-2Suche in Google Scholar

Helffrich, G. (2000) Topography of the transition zone seismic discontinuity. Reviews of Geophysics, 38, 141–158.10.1029/1999RG000060Suche in Google Scholar

Herzberg, C., Asimow, P.D., Arndt, N., Niu, Y., Lesher, C.M., Fitton, J.G., Cheadle, M.J., and Saunders, A.D. (2007) Temperatures in ambient mantle and plumes: Constraints from basalts, picrites, and komatiites. Geochemistry, Geophysics, Geosystems, 8, 2, 10.1029/2006GC001390.Suche in Google Scholar

Inoue, T., Irifue, T., Higo, T., Sanehira, T., Sueda, Y., Yamada, A., Shinmei, T., Yamazaki, D., Ando, J., Funakoshi, K., and Utsumi, W. (2006) The phase boundary between wadsleyite and ringwoodite in Mg2SiO4 determined by in situ X-ray diffraction. Physics and Chemistry of Minerals, 33, 106–114.10.1007/s00269-005-0053-ySuche in Google Scholar

Inoue, T., Wada, T., Sasaki, R., and Yurimoto, H. (2010a) Water partitioning in the Earth’s mantle. Physics of the Earth and Planetary Interiors, 183, 245–251.10.1016/j.pepi.2010.08.003Suche in Google Scholar

Inoue, T., Ueda, T., Yanimoto, Y., Yamada, A., and Irifune, T. (2010b) The effect of water on the high-pressure phase boundaries in the system Mg2SiO4-Fe2SiO4. Journal of Physics: Conference Series, 2015, 012101.10.1088/1742-6596/215/1/012101Suche in Google Scholar

Ita, J., and Stixrude, L. (1992) Petrology, elasticity, and composition of the mantle transition zone. Journal of Geophysical Research, 97, B, 5, 6849–6866.10.1029/92JB00068Suche in Google Scholar

Katsura, T., and Ito, E. (1989) The system Mg2SiO4-Fe2SiO4 at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel. Journal of Geophysical Research, 94, 15,663–15,670.10.1029/JB094iB11p15663Suche in Google Scholar

Katsura, T., Yamada, H., Nishikawa, O., Song, M., Kubo, A., Shinmei. T., Yokoshi, S., Aizawa, Y., Yoshino, T., Walter, M.J., and Ito, E. (2004) Olivine-wadsleyite transition in the system (Mg,Fe)2SiO4. Journal of Geophysical Research, 109, 10.1029/2003JB002438.Suche in Google Scholar

Kennett, B.L.N., and Engdahl, E.R. (1991) Travel times for global earthquake location and phase identification. Geophysical Journal International, 105, 429–465.10.1111/j.1365-246X.1991.tb06724.xSuche in Google Scholar

Kubo, T., Shimojuku, and, A., Ohtani, E. (2004) Mg-Fe interdiffusion rates in wadsleyite and the diffusivity jump at the 410-km discontinuity. Physics and Chemistry of Minerals, 31, 456–464.10.1007/s00269-004-0412-0Suche in Google Scholar

Liu, W., Kung, J., Li, B., Nishiyama, N., Wang, Y. (2009) Elasticity of (Mg0.87Fe0.13)2SiO4 wadsleyite to 12 GPa and 1073 K. Physics of the Earth and Planetary Interiors, 174, 98–104.10.1016/j.pepi.2008.10.020Suche in Google Scholar

McKenzie, D., and Bickle, M.J. (1988) The volume and composition of melt generated by extension of the lithosphere. Journal of Petrology, 29, 623–679.10.1093/petrology/29.3.625Suche in Google Scholar

Morishima, E., Kato, Suto, M., Ohtani, E., Urakawa, S., Utsumi, W., Shimomura, O., and Kikekgawa, T. (1994) The phase boundary between α-and β-Mg2SiO4 determined by in situ X-ray observation. Science, 265, 1202–1203.10.1126/science.265.5176.1202Suche in Google Scholar PubMed

Mrosko, M., Koch-Müller, M., McCammon, C., Rhede, D., Smyth, J.R., and Wirth, R. (2015) Water, iron, redox environment: effects on the wadsleyite-ringwoodite phase transition. Contributions to Mineralogy and Petrology, 170, 9, 10.1007/s00410-015-1163-2.Suche in Google Scholar

Nishihara, Y., Takahashi, E., Matsukage, K.N., Iguchi, T., Nakayama, K., and Funakoshi, K. (2004) Thermal equation of state of (Mg0.91Fe0.09)2SiO4 ring-woodite. Physics of the Earth and Planetary Interiors, 143-144, 33–46.10.1016/j.pepi.2003.02.001Suche in Google Scholar

Nishiyama, N., Irifune, T., Inoue, T., Ando, J.I., and Funakoshi, K.I. (2004) Precise determination of phase relations in pyrolite across the 660 km seismic discontinuity by in situ X-ray diffraction and quench experiments. Physics of the Earth and Planetary Interiors, 143, 185–199.10.1016/j.pepi.2003.08.010Suche in Google Scholar

Saikia, A., Frost, D.J., and Rubie, D.C. (2008) Splitting of the 520-kilometer Seismic Discontinuity and Chemical Heterogeneity in the Mantle. Science, 319, 1515–1518.10.1126/science.1152818Suche in Google Scholar PubMed

Shearer, P.M. (1990) Seismic imaging of upper-mantle structure with new evidence for a 520-km discontinuity. Nature, 344, 121–126.10.1038/344121a0Suche in Google Scholar

Shearer, P.M. (1991) Constrains on upper mantle discontinuity from observations of long-period reflected and converted phases. Journal of Geophysical Research, 96, 18,147–18,182.10.1029/91JB01592Suche in Google Scholar

Speziale, S., Zha, C., Duffy, T.S., Hemley, R.J., and Mao, H. (2001) Quasi-hydrostatic compression of magnesium oxide to 52 GPa: Implications for the pressure-volume-temperature equation of state. Journal of Geophysical Research, 106, 515–528.10.1029/2000JB900318Suche in Google Scholar

Stixrude, L. (1997) Structure and sharpness of phase transitions and mantle discontinuities. Journal of Geophysical Research, 102, B, 7, 14,835–14,852.10.1029/97JB00550Suche in Google Scholar

Sun, W., Yoshino, T., Sakamoto, N., and Yurimoto, H. (2015) Hydrogen self-diffusivity in single crystal ringwoodite: Implications for water content and distribution in the mantle transition zone. Geophysical Research Letters, 10.1002/2015GL064486.Suche in Google Scholar

Sun, W., Yoshino, T., Sakamoto, N., and Yurimoto, H. (2018) Supercritical fluid in the mantle transition zone deduced from H/D interdiffusion of wadsleyite. Earth and Planetary Science Letters, 484, 309–317.10.1016/j.epsl.2017.12.032Suche in Google Scholar

Suzuki A., Othtani, E., Morishima, H., Kubo, T., Kanbe, Y., and Kondo, T. (2000) In situ determination of the phase boundary between wadsleyite and ringwoodite in Mg2SiO4. Geophysical Research Letters, 27, 803–806.10.1029/1999GL008425Suche in Google Scholar

Tange, Y., Nishihara, Y., and Tsuchiya, T. (2009) Unified analyses for P-V-T equation of state of MgO: A solution for pressure-scale problems in high P-T experiments. Journal of Geophysical Research, 114, B03208, 10.1029/2008JB005813.Suche in Google Scholar

Tian, Y., Zhu, H., Zhao, D., Liu, C., Feng, X., Liu, T., and Ma, J. (2016) Mantle transition zone structure beneath the Changbai volcano: Insight into deep slab dehydration and hot upwelling near the 410 km discontinuity. Journal of Geophysical Research, 121, 5794–5808, 10.1002/2016JB012959.Suche in Google Scholar

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. The Review of High Pressure Science and Technology, 7, 1484–1486.10.4131/jshpreview.7.1484Suche in Google Scholar

Zhang, J., and Herzberg, C. (1994) Melting experiments on anhydrous peridotite KLB-1 from 5.0 to 22.5 GPa. Journal of Geophysical Research, 99, 17,729–17,742.10.1029/94JB01406Suche in Google Scholar

Received: 2018-09-24
Accepted: 2019-01-15
Published Online: 2019-03-24
Published in Print: 2019-04-24

© 2019 Walter de Gruyter GmbH, Berlin/Boston

Artikel in diesem Heft

  1. Introduction
  2. Deep carbon cycle through five reactions
  3. Earth in five reactions: Grappling with meaning and value in science
  4. In-situ iron isotope analyses reveal igneous and magmatic-hydrothermal growth of magnetite at the Los Colorados Kiruna-type iron oxide-apatite deposit, Chile
  5. Carbon and nitrogen isotopes and mineral inclusions in diamonds from chromitites of the Mirdita ophiolite (Albania) demonstrate recycling of oceanic crust into the mantle
  6. Geochronology and trace element mobility in rutile from a Carboniferous syenite pegmatite and the role of halogens
  7. The incorporation of chlorine into calcium amphibole
  8. Crystal size distribution of amphibole grown from hydrous basaltic melt at 0.6–2.6 GPa and 860–970 °C
  9. Role of micropores, mass transfer, and reaction rate in the hydrothermal alteration process of plagioclase in a granitic pluton
  10. Lead diffusion in CaTiO3: A combined study using Rutherford backscattering and TOF-SIMS for depth profiling to reveal the role of lattice strain in diffusion processes
  11. On growth and form of etched fission tracks in apatite: A kinetic approach
  12. High-pressure behavior of liebenbergite: The most incompressible olivine-structured silicate
  13. Phase transition of wadsleyite-ringwoodite in the Mg2SiO4-Fe2SiO4 system
  14. Cation ordering, valence states, and symmetry breaking in the crystal-chemically complex mineral chevkinite-(Ce): X-ray diffraction and photoelectron spectroscopy studies and mechanisms of Nb enrichment
  15. Meyrowitzite, Ca(UO2)(CO3)2⋅5H2O, a new mineral with a novel uranyl-carbonate sheet
  16. Letter
  17. Discovery of the first natural hydride
  18. Synthesis of pigeonites for spectroscopic studies
  19. Presentation of the 2018 Roebling Medal of the Mineralogical Society of America to E. Bruce Watson
  20. Acceptance of the 2018 Roebling Medal of the Mineralogical Society of America
  21. Presentation of the Dana Medal of the Mineralogical Society of America for 2018 to Jörg Hermann
  22. Acceptance of the Dana Medal of the Mineralogical Society of America for 2018
  23. New Mineral Names
  24. Book Review
Heruntergeladen am 21.4.2026 von https://www.degruyterbrill.com/document/doi/10.2138/am-2019-6823/html
Button zum nach oben scrollen