Structure and density of molten fayalite at high pressure

Geochimica et Cosmochimica Acta

Volumn 118, Issue , 2013, Pages 118-128

  Sanloup, C ^a   Drewitt, J W E ^a   Crepisson C ^b   Kono, Y ^c   Park, C ^c   McCammon, C ^d   Hennet, L ^e   Brassamin, S ^e   Bytchkov, A ^f  

^a UNIVERSITY OF EDINBURGH   (United Kingdom)

^b Sorbonne Universités   (France)

^c GEOPHYSICAL LABORATORY   (United States)

^d UNIVERSITÄT BAYREUTH   (Germany)

^e UNIVERSITÉ D'ORLÉANS   (France)

^f INSTITUT LAUE LANGEVIN   (France)

Author keywords

[No Author keywords available]

Indexed keywords

COMPRESSIBILITY; EQUATION OF STATE; FAYALITE; HIGH PRESSURE; IN SITU STRESS; MANTLE STRUCTURE; P-T CONDITIONS; SILICATE; X-RAY DIFFRACTION;

EID: 84879012185     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gca.2013.05.012     Document Type: Article

References (47)

1. 4. Geophys. Res. Lett. 1992, 19:1169-1172.
2. 4 at high pressure. Geophys. Res. Lett. 1992, 19:1173-1176.
3. 4. J. Geophys. Res. 1967, 72:679-686.
4. 9 glasses: an investigation utilizing Raman and NMR spectroscopy of glasses and crystalline materials. Chem. Geol. 2004, 213:137-151.
5. Baratoux D., Toplis M.J., Monnereau M., Gasnault O. Thermal history of Mars inferred from orbital geochemistry of volcanic provinces. Nature 2011, 472:338-342.
6. Benmore C.J., Soignard E., Amin S.A., Guthrie M., Shastri S.D., Lee P.L., Yarger J.L. Structural and topological changes in silica glass at pressure. Phys. Rev. B 2010, 81:054105.
7. Cahill J.T.S., Lucey P.G., Wieczorek M.A. Compositional variations of the lunar crust: results from radiative transfer modeling of central peak spectra. J. Geophys. Res. 2009, 114:E09001.
8. Chen G.Q., Ahrens T.J., Stolper E.M. Shock-wave equation of state of molten and solid fayalite. Phys. Earth Planet. Inter. 2002, 134:35-52.
9. 3 perovskite at high pressure and temperature. Nature 2002, 419:824-826.
10. 2 liquid system in Earths lowermost mantle from first principles. Earth Planet. Sci. Lett. 2013, 361:58-63.
11. 4 liquid at high pressure. Geochim. Cosmochim. Acta 2008, 72:1427-1441.
12. Drewitt J.W.E., Jahn S., Cristiglio V., Bytchkov A., Leydier M., Brassamin S., Fischer H.E., Hennet L. The structure of liquid calcium aluminates as investigated using neutron and high energy X-ray diffraction in combination with molecular dynamics simulation methods. J. Phys. Condens. Matter 2011, 23:155101.
13. Egelstaff P.A. An Introduction to the Liquid State 1994, Oxford University Press, Oxford.
14. Eggert J.H., Weck G., Loubeyre P., Mezouar M. Quantitative structure factor and density measurements of high-pressure in diamond anvil cells by X-ray diffraction: argon and water. Phys. Rev. B 2002, 65:174105-1-174105-12.
15. Funamori N., Yamamoto S., Yagi T., Kikegawa T. Exploratory studies of silicate melt structure at high pressures and temperatures by in situ X-ray diffraction. J. Geophys. Res. 2004, 109:B03203.
16. 3. Geochim. Cosmochim. Acta 2008, 72:1222-1230.
17. Guillot B., Sator N. A computer simulation study of natural silicate melts. Part II: High pressure properties. Geochim. Cosmochim. Acta 2007, 71:4538-4556.
18. Hajdu F. Revised parameters of the analytic fits for coherent and incoherent scattered X-ray intensities of the first 36 atoms. Acta Crystallogr. 1972, 250-252.
19. Hosemann R., Bagchi S.N. Direct Analysis of Diffraction by Matter 1962, North-Holland, Amsterdam.
20. Hsu L.C. Melting of fayalite up to 40 kilobars. J. Geophys. Res. 1967, 72:4235-4244.
21. Hubbell J. and Seltzer S. (2004) Tables of X-ray mass attenuation coefficients and mass energy-absorption coefficients (version 1.4). Available from: http://physics.nist.gov/xaamdi.
22. 4 liquid: reduced coordination of ferrous iron. Science 1993, 262:229-233.
23. Jackson W.E., Farges F., Yeager M., Mabrouk P.A., Rossano S., Waychunas G.A., Solomon E.I., Brown G.E. Multi-spectroscopic study of Fe(II) in silicate glasses: implications for the coordination environment of Fe(II) in silicate melts. Geochim. Cosmochim. Acta 2005, 69:4315-4332.
24. Kaplow R., Strong S.L., Averbach B.L. Radial density functions for liquid mercury and lead. Phys. Rev. 1965, 138:A1336.
25. Keppler H., Rubie D.C. Pressure-induced coordination changes of transition-metal ions in silicate melts. Nature 1993, 364:54-56.
26. Kohara S., Akola J., Morita H., Suzuya K., Weber J.K.R., Wilding M.C., Benmore C.J. Relationship between topological order and glass forming ability in densely packed enstatite and forsterite composition glasses. PNAS 2011, 108:14780-14785.
27. Kono Y., Irifune T., Higo Y., Inoue T., Barnhoorn A. P-V-T relation of MgO derived by simultaneous elastic wave velocity and in situ X-ray measurements: a new pressure scale for the mantle transition region. Phys. Earth Planet. Int. 2010, 183:196-211.
28. Krogh-Moe J. A method for converting experimental X-ray intensities to an absolute scale. Acta Crystallogr. 1956, 9:951-953.
29. Lee C.-T.A., Luffi P., Höink T., Li J., Dasgupta R., Hernlund J. Upside-down differentiation and generation of a primordial lower mantle. Nature 2010, 463:930-935.
30. Nittler L.R., Starr R.D., Weider S.Z., McCoy T.J., Boynton W.V., Ebel D.S., Ernst C.M., Evans L.G., Goldsten J.O., Hamara D.K., Lawrence D.J., McNutt R.L., Schlemm C.E., Solomon S.C., Sprague A.L. The major-element composition of Mercurys surface from MESSENGER X-ray spectrometry. Science 2011, 333:1847-1850.
31. Norman N. The Fourier transform method for normalizing intensities. Acta Crystallogr. 1957, 10:370-373.
32. 4 up to about 200kbar. Earth Planet. Sci. Lett. 1984, 71:94-103.
33. Rivers M.L., Carmichael I.S.E. Ultrasonic studies of silicate melts. J. Geophys. Res. 1987, 92:9247-9270.
34. 57Fe Mössbauer data of alumino-silicate glasses. Phys. Chem. Miner. 2008, 35:77-93.
35. Sakamaki T., Wang Y., Park C., Yu T., Shen G. Structure of jadeite melt at high pressures up to 4.9GPa. J. Appl. Phys. 2012, 111:112623.
36. Salmon P.S. Real space manifestation of the first sharp diffraction peak in the structure factor of liquid and glassy materials. Proc. Math. Phys. Sci. 1994, 445:351-365.
37. 2 under high pressure. Phys. Rev. Lett. 2008, 101:255502.
38. 2 glass up to 100GPa. Phys. Rev. B 2010, 82:184102.
39. 5). Geophys. Res. Lett. 1999, 26:2521-2523.
40. 4 melt and the density of Fe-bearing silicate melts from 0-161GPa. J. Geophys. Res. 2012, 117:B10206.
41. van Kan Parker M., Sanloup C., Sator N., Guillot B., Tronche E.J., Perrillat J.-P., Mezouar M., Rai N., van Westrenen W. Neutral buoyancy of titanium-rich melts in the deep lunar interior. Nat. Geosci. 2012, 5:186-189.
42. 2 system. Trans. JIM 1978, 21:51-62.
43. 2+ in molten alkali silicates. Nature 1988, 332:251-253.
44. Weigel C., Cormier L., Calas G., Galoisy L., Bowron D.T. Nature and distribution of iron sites in a sodium silicate glass investigated by neutron diffraction and EPSR simulation. J. Non-Cryst. Solids 2008, 354:5378-5385.
45. Wilke M. Fe in magma - an overview. Ann. Geophys. 2005, 48:609-617.
46. Wilke M., Farges F., Partzsch G.M., Schmidt C., Behrens H. Speciation of Fe in silicate glasses and melts by in-situ XANES spectroscopy. Am. Miner. 2007, 92:44-56.
47. Yarger J.L., Smith K.H., Nieman R.A., Diefenbacher J., Wolf G.H., Poe B.T., McMillan P.F. Al coordination changes in high-pressure aluminosilicate liquids. Science 1995, 270:1964-1967.