Pressure-induced change in the compressional behavior of the O-H bond in chrysotile: A Raman high-pressure study up to 4.5 GPa

American Mineralogist

Volumn 92, Issue 8-9, 2007, Pages 1456-1463

  Mizukami, Tomoyuki ^a,b   Kagi, Hiroyuki ^a   Wallis, Simon R ^b   Fukura, Satoshi ^a  

^a UNIVERSITY OF TOKYO   (Japan)

^b NAGOYA UNIVERSITY   (Japan)

Author keywords

Chrysotile; Compressional behavior of sheet silicate; High pressure Raman spectroscopy; O H bond; Pressure scale

Indexed keywords

COMPRESSIBILITY; NANOFIBERS; SILICATES;

CHRYSOTILE; COMPRESSIONAL; HIGH-PRESSURE RAMAN SPECTROSCOPIES; O-H BOND; PRESSURE SCALE;

SERPENTINE;

ASBESTOS; COMPRESSIBILITY; DIAMOND ANVIL CELL; HIGH PRESSURE; PHASE TRANSITION; RAMAN SPECTROSCOPY;

EID: 38849114963     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2007.2489     Document Type: Article

References (45)

1. Auzende, A-L., Daniel, I., Reynard, B., and Lemaire, C. (2004) High-pressure behaviour of serpentine minerals: a Raman spectroscopic study. Physics and Chemistry of Minerals, 31, 269-277.
2. Baronnet, A. and Devouard, B. (1996) Topology and crystal growth of natural chrysotile and polygonal serpentine. Journal of Crystal Growth, 166, 952-960.
3. Bostock, M.G., Hyndman, R.D., Rondenay, S., and Peacock, S.M. (2002) An inverted continental Moho and serpentinization of the forearc mantle. Nature, 417, 536-538.
4. 3+ substitution on high-pressure stability. American Mineralogist, 88, 99-108.
5. Dera, P., Prewitt, C.T., Japel, S., Bish, L.D., and Johnston, C.T. (2003) Pressure-controlled polytypism in hydrous layered materials. American Mineralogist, 88, 1428-1435.
6. Dobson, D.P., Meredith, P.G., and Boon, S.A. (2002) Simulation of subduction zone seismicity by dehydration of serpentine. Science, 298, 1407-1410.
7. Dórdony, I. and Buseck, P.R. (2004a) Serpentine close-up and intimate: An HRTEM view. International Geology Review, 46, 507-527.
8. Dórdony, I. (2004b) Lizardite-chlorite structural relationships and an inferred high-pressure lizardite polytype. American Mineralogist, 89, 1631-1639.
9. 2. American Mineralogist, 80, 222-230.
10. Evans, B.W. (2004) The serpentine multisystem revisited: Chrysotile is metastable. International Geology Review, 46, 479-506.
11. Falini, G., Foresti, E., Gazzano, M., Gualtieri, A.F., Leoni, M., Lesci, I.G., and Roveri, N. (2004) Tubular-shaped stoichiometric chrysotile nanocrystals. Chemistry, 10, 3043-3049.
12. Freyer, P., Ambos, E.L., and Hussong, D.M. (1985) Origin and emplacement of Mariana forearc seamounts. Geology, 13, 774-777.
13. Fukura, S., Mizukami, T., Odake, S., and Kagi, H. (2006) Factors determining the stability, resolution, and precision of a conventional Raman spectrometer. Applied Spectroscopy, 60, 946-950.
14. Guillot, S., Hattori, K.H., de Sigoyer, J., Ngler, T., and Auzende A.-L. (2001) Evidence of hydration of the mantle wedge and its role in the exhumation of eclogites. Earth and Planetary Science Letters, 193, 115-127.
15. Hofmeister, A.M., Cynn, H., Burnley, P.C., and Meade, C. (1999) Vibrational spectra of dense, hydrous magnesium silicates at high pressure: Importance of the hydrogen bond angle. American Mineralogist, 84, 454-464.
16. Holland, T.J.B. and Powell, R. (1998) An internally consistent thermodynamic data set for phases of petrological interest. Journal of Metamorphic Geology, 16, 309-343.
17. Holtz, M., Solin, S.A., and Pinnavaia, T.J. (1993) Effect of pressure on the Raman vibrational modes of layered aluminosilicate compounds. Physical Review B, 48, 13312-13317.
18. Izraeli, E.S., Harris, J.W., and Navon, O. (1999) Raman barometry of diamond formation. Earth and Planetary Science Letters, 173, 351-360.
19. Johnston, C.T., Wang, S-L., Bish, D.L., Dera, P., Agnew, S.F., and Kenney, J.W. III. (2002) Novel pressure-induced phase transformations in hydrous layered materials. Geophysical Research Letters, 29, DOI: 10.1029/2002GL015402.
20. Jung, H.-Y., Green II, H.W., and Dobrzhinetskaya, L.F. (2004) Intermediate-depth earthquake faulting by dehydration embrittlement with negative volume change. Nature, 428, 545-549.
21. Kawamoto, T., Ochiai, S., and Kagi, H. (2004) Changes in the structure of water deduced from the pressure dependence of the Raman OH frequency. Journal of Chemical Physics, 120, 5867-5870.
22. Kleppe, A.L., Jephcoat, A.P., and Welch, M.D. (2003) The effect of pressure upon hydrogen bonding in chlorite: a Raman spectroscopic study of clinochlore to 26.5 GPa. American Mineralogist, 88, 567-573.
23. Kloprogge, J.T., Frost, R.L., and Rintoul, L. (1999) Single crystal Raman microscopic study of the asbestos mineral chrysotile. Physical Chemistry Chemical Physics, 1, 2559-2564.
24. Komatsu, K., Kagi, H., Okada, T., Kuribayashi, T., Parise, J.B., and Kudoh, Y. (2005) Pressure dependence of OH stretching mode in F-rich natural topaz and topaz-OH. American Mineralogist, 90, 266-270.
25. Liu, Z.-X., Lager, G.A., Hemley, R.J., and Ross, N.L. (2003) Synchrotron infrared spectroscopy of OH-chondrodite and OH-clinohumite at high pressure. American Mineralogist, 88, 1412-1415.
26. Mamontov, E., Kumzerov, Y.A., and Vakhrushev, S.B. (2005) Translational dynamics of water in the nanochannels of oriented chrysotile asbestos fibers. Physical Review E, 71, 061502.
27. Mellini, M. and Zanazzi, P.F. (1987) Crystal structures of lizardite 1T and lizardite-2H1 from Coli, Italy. American Mineralogist, 72, 943-948.
28. Mizukami, T. and Wallis, S.R. (2005) Structural and petrological constraints on the tectonic evolution of the garnet-lherzolite facies Higashi-akaishi peridotite body, Sanbagawa belt, SW Japan. Tectonics, 24, TC6012, DOI: 10.1029/2004TC001733.
29. Muller, M.R., Robinson, C.J., Minshull, T.A., White, R.S., and Bickle, M.J. (1997) Thin crust beneath ocean drilling program borehole 735B at the Southwest Indian Ridge? Earth end Planetary Science Letters, 148, 93-107.
30. Okada, T., Komatsu, K., Kawamoto, T., Yamanaka, T., and Kagi, H. (2005) Pressure response of Raman spectra of water and its implication to the change in hydrogen bond interactions. Spectrochimica Acta A, 61, 2423-2427.
31. Peacock, S.M. (1996) Thermal and petrologic structure of subduction zones. AGU Geophysical Monograph, 96, 119-133.
32. Pellenq, R.J., Auzende, A., Devouard, B., Baronnet, A., and Grauby, O. (2005) Free energy minimization calculations of lizardite at variable pressures and temperatures. Abstract. AGU Fall Meeting, EOS Transaction, 86.
33. Piermarini, G.L., Block, S., Barnett, J.D., and Forman, R.A. (1975) Calibration of the pressure dependence of the R1 ruby fluorescence line to 195 kbar. Journal of Applied Physics, 46, 2774-2780.
34. Rayner, J.H. and Brown, G. (1973) The crystal structure of talc. Clays and Clay Minerals, 21, 103-114.
35. Rüpke, L.H., Morgan, J.P., Hort, M., and Connolly, J.A.D. (2004) Serpentine and the subduction zone water cycle. Earth and Planetary Science Letters, 223, 17-34.
36. Stixrude, L. (2002) Talc under tension and compression: Spinodal instability, elasticity, and structure. Journal of Geophysical Research, 107(B12), 2327, DOI: 10.1029/2001JB001684.
37. Sobolev, N.V., Fursenko, B.A., Goryainov, S.V., Shu, J., Hemley, R.J., Mao, H.-K., and Boyd, F.R. (2000) Fossilized high pressure from the Earth's deep interior: The coesite-in-diamond barometer. Geology, 97, 11875-11879.
38. Ulmer, P. and Trommsdorff, V. (1995) Serpentine stability to mantle depths and subduction-related magmatism. Science, 268, 858-861.
39. Ulmer, P. (1999) Phase relations of hydrous mantle subducting to 300 km. In Y. Fei, C.M. Bertka, and B.O. Mysen, Eds., Mantle petrology: Field observations and high pressure experimentation, 6, p. 259-281. Geochemical Society Special Publication, The Geochemical Society, Houston, Texas.
40. Welch, M.D. and Marshall, W.G. (2001) High-pressure behavior of clinochlore. American Mineralogist, 86, 1380-1386.
41. Whittaker, E.J.W. (1957) The structure of chrysotile. V. Diffuse reflections and fibre texture. Acta Crystallographica, 10, 149.
42. Wicks, F.J. and O'Hanley, D.S. (1988) Serpentine minerals: structures and petrology. In S.W. Bailey, Ed., Hydrous phyllosilicates, 19, p. 91-167. Reviews in Mineralogy, Mineralogical Society of America, Chantilly, Virginia.
43. 2O (MSH). Lithos, 41, 213-227.
44. Yamamoto, J., Kagi, H., Kaneoka, I., Lai, Y., Prikhod'ko, V.S., and Arai, S. (2002) Fossil pressures of fluid inclusions in mantle xenoliths exhibiting rheology of mantle minerals using micro-Raman spectroscopy. Earth and Planetary Science Letters, 198, 511-519.
45. Zedgenizov, D.A., Kagi, H., Shatsky, V.S., and Sobolev, N.V. (2004) Carbonatitic melts in cuboid diamonds from Udachnaya kimberlite pipe (Yakutia): evidence from vibrational spectroscopy. Mineralogical Magazine, 68, 61-73.