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Synthesis and crystal structure of chromium-bearing anhydrous wadsleyite

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Abstract

A chromium-bearing wadsleyite (Cr-Wad) was synthesized in the model system Mg2SiO4–MgCr2O4 at 14 GPa and 1600 °C and studied from the chemical and structural point of views. Microprobe data gave the formula Mg1.930Cr0.120Si0.945O4, on the basis of 4 oxygen atoms. The crystal structure has been studied by single-crystal X-ray diffraction. The orthorhombic unit-cell parameters are: a = 5.6909(5) Å, b = 11.4640(10) Å, c = 8.2406(9) Å, V = 537.62(9) Å3, Z = 8. The structure, space group Imma, was refined to R 1 = 5.99% in anisotropic approximation using 1135 reflections with F o > 4σ(F o) and 43 parameters. Chromium was found to substitute for both Mg at the octahedral sites and Si at the tetrahedral site, according to the reaction VIMg2+ + IVSi4+ = VICr3+ + IVCr3+. On the whole, the structural topology is nearly identical to that of pure wadsleyite. The successful synthesis of Cr-Wad may be important for the thermobarometry of mantle phase associations.

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References

  • Arai S (2010) Possible recycled origin for ultrahigh-pressure chromitites in ophiolites. J Miner Petrol Sci 105:280–285

    Article  Google Scholar 

  • Bindi L, Sirotkina EA, Bobrov AV, Irifune T (2015) Structural and chemical characterization of Mg[(Cr,Mg)(Si,Mg)]O4, a new post-spinel phase with sixfold-coordinated silicon. Am Miner 100:1633–1636

    Article  Google Scholar 

  • Bolfan-Casanova N, Muñoz M, McCammon C, Deloule E, Férot A, Demouchy S, France L, Andrault D, Pascarelli S (2012) Ferric iron and water incorporation in wadsleyite under hydrous and oxidizing conditions: a XANES, Mössbauer, and SIMS study. Am Miner 97:1483–1493

    Article  Google Scholar 

  • Dobrzhinetskaya L, Green HW, Wang S (1996) Alpe Arami: a peridotite massif from depths of more than 300 kilometers. Science 271:1841–1845

    Article  Google Scholar 

  • Dymshits AM, Litasov KD, Sharygin IS, Shatskiy A, Ohtani E, Suzuki A, Funakoshi K (2014) Thermal equation of state of majoritic knorringite and its significance for continental upper mantle. J Geophys Res Solid Earth 119:8034–8046

    Article  Google Scholar 

  • Griffin WL, Afonso JC, Belousova EA, Gain SE, Gong XH, Gonzalez-Jimenez JM, Satsukawa T (2016) Mantle recycling: transition zone metamorphism of Tibetan ophiolitic peridotites and its tectonic implications. J Petrol 57:655–684

    Article  Google Scholar 

  • Gudfinnsson GH, Wood BJ (1998) The effect of trace elements on the olivine–wadsleyite transformation. Am Miner 83:1037–1044

    Article  Google Scholar 

  • Harte B (2010) Diamond formation in the deep mantle: the record of mineral inclusions and their distribution in relation to mantle dehydration zones. Min Mag 74(2):189–215

    Article  Google Scholar 

  • Hazen RM, Weinberger MB, Yang H, Prewitt CT (2000) Comparative high-pressure crystal chemistry of wadsleyite, β-(Mg1–xFex)2SiO4, with x = 0 and 0.25. Am Miner 85(5–6):770–777

    Article  Google Scholar 

  • Ibers JA, Hamilton WC (eds) (1974) International tables for X-ray crystallography. vol. IV. The Kynoch Press, Birmingham

    Google Scholar 

  • Inoue T, Yurimoto Y, Kudoh T (1995) Hydrous modified spinel, Mg1.75SiH0.504: a new water reservoir in the mantle transition region. Geophys Res Lett 22:117–120

    Article  Google Scholar 

  • Irifune T, Kurio A, Sakamoto S, Inoue T, Sumiya H, Funakoshi K (2004) Formation of pure polycrystalline diamond by direct conversion of graphite at high pressure and high temperature. Phys Earth Planet Inter 143:593–600

    Article  Google Scholar 

  • Katsura T, Ito E (1989) The system Mg2SiO4–Fe2SiO4 at high pressure and temperatures: precise determination of stabilities of olivine, modified spinel and spinel. J Geophys Res 94:15663–15670

    Article  Google Scholar 

  • Oxford Diffraction (2009) CrysAlisPro. Oxford Diffraction Ltd, Abingdon

  • Pushcharovsky DY, Pushcharovsky YM (2012) The mineralogy and the origin of deep geospheres: a review. Earth Sci Rev 113:94–109

    Article  Google Scholar 

  • Ringwood AE (1966) The chemical composition and origin of the earth. In: Hurley PM (ed) Advances in earth science. M.I.T. Press, Cambridge, pp 287–356

  • Sheldrick GM (2008) A short history of SHELX. Acta Cryst Section A. Found Crystallography 64(1):112–122

    Article  Google Scholar 

  • Sirotkina EA, Bobrov AV, Bindi L, Irifune T (2015) Phase relations and formation of chromium‑rich phasesthe system Mg4Si4O12–Mg3Cr2Si3O12 at 10–24 GPa and 1,600 °C. Contrib Mineral Petrol 169:2. doi:10.1007/s00410-014-1097-0

    Article  Google Scholar 

  • Smyth JR, Bolfan-Casanova N, Avignant D, El-Ghozzi M, Himer SM (2014) Tetrahedral ferric iron in oxidized hydrous wadsleyite. Am Miner 99:458–466

    Article  Google Scholar 

  • Stalder R (2004) Influence of Fe, Cr and Al on hydrogen incorporation in orthopyroxene. Eur J Miner 16(5):703–711

    Article  Google Scholar 

  • Yamada A, Inoue T, Irifune T (2004) Melting of enstatite from 13 to 18 GPa under hydrous conditions. Phys Earth Planet Inter 147:45–56

    Article  Google Scholar 

  • Yufeng R, Fangyuan C, Jingsui Y, Yuanhong G (2008) Exsolutions of diopside and magnetite in olivine from mantle dunite, Luobusa ophiolite, Tibet, China. Acta Geol Sinica 82:377–384

    Article  Google Scholar 

  • Zhang RY, Shu JF, Mao HK, Liou JG (1999) Magnetite lamellae in olivine and clinohumite from Dabie UHP ultramafic rocks, central China. Am Miner 84(4):564–569

    Article  Google Scholar 

  • Zhang L, Smyth JR, Allaz J, Kawazoe T, Jacobsen SD, Jin Z (2016) Transition metals in the transition zone: crystal chemistry of minor element substitution in wadsleyite. Am Miner 101:2322–2330

    Article  Google Scholar 

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Acknowledgements

The research was supported by the Russian Science Foundation (project no. 17-17-01169 to AB and ES). Structural studies were partly supported by the Foundation of the President of the Russian Federation (grant no. MK-1277.2017.5 to ES).

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Correspondence to E. A. Sirotkina.

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Sirotkina, E.A., Bindi, L., Bobrov, A.V. et al. Synthesis and crystal structure of chromium-bearing anhydrous wadsleyite. Phys Chem Minerals 45, 361–366 (2018). https://doi.org/10.1007/s00269-017-0926-x

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  • DOI: https://doi.org/10.1007/s00269-017-0926-x

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