Mechanisms of transformation and deformation in Mg1.8Fe0.2SiO4 olivine and wadsleyite under non-hydrostatic stress

Physics of the Earth and Planetary Interiors

Volumn 108, Issue 1, 1998, Pages 33-48

  Dupas Bruzek, Catherine ^a   Sharp, Thomas G ^a,c   Rubie, David C ^a   Durham, William B ^b  

^a UNIVERSITÄT BAYREUTH   (Germany)

^b LAWRENCE LIVERMORE NATIONAL LABORATORY   (United States)

^c ARIZONA STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

DEFORMATION; HIGH PRESSURE; OLIVINE; TRANSFORMATION; WADSLEYITE;

EID: 0032577198     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0031-9201(98)00086-7     Document Type: Article

References (70)

1. Bai Q., Kohlstedt D.L. High temperature creep of olivine single crystals: 2. Dislocations structures. Tectonophysics. 206:1992;1-29.
2. Bai Q., Mackwell S.J., Kohlstedt D.L. High temperature creep of olivine single crystals: 1. Mechanical results for buffered samples. J. Geophys. Res. 96:1991;2441-2463.
3. 4 wadsleyite under subduction zone conditions. Phys. Earth Planet. Int. 86:1994;45-67.
4. 4 at 15 GPa. Phys. Chem. Minerals. 18:1992;343-358.
5. Burnley P.C. The fate of olivine in subducting slabs: a reconnaissance study. Am. Mineral. 80:1995;1293-1301.
6. 4 and its implications for deep focus earthquakes. J. Geophys. Res. 96:1991;425-443.
7. 4. J. Geophys. Res. 100:1995;17715-17723.
8. Bussod G.Y., Katsura T., Rubie D.C. The large volume multi-anvil press as a high P-T deformation apparatus. Pageoph. 141:1993;579-599.
9. Canil D. Stability of clinopyroxene at pressure-temperature conditions of the transition region. Phys. Earth Planet. Int. 86:1994;25-34.
10. é Lallemant, 1970
11. Carter N.L., Avé Lallemant H.G. High temperature flow of dunite and peridotite. Geol. Soc. Am. Bull. 81:1970;2181-2202.
12. Daessler R., Yuen D.A., Karato S.I., Riedel M.R. Two dimensional thermo kinetic model for the olivine-spinel phase transition in subducting slabs. Phys. Earth Planet. Int. 94:1996;217-239.
13. Doukhan, N., Doukhan, J.C., Fitz Gerald, J.D., Chopra, P.N., Paterson, M.S., 1984. A TEM microstructural study of experimentally deformed Anita Bay dunite. In: Bradt, R.C., Tressler, R.E. (Eds.), Deformation of Ceramic Materials II. Plenum, New York, pp. 307-319.
14. Dupas C., Doukhan N., Doukhan J.C., Green H.W., Young T.E. Analytical electron microscopy study of a synthetic peridotite experimentally deformed in the β olivine stability field. J. Geophys. Res. 99:1994;15821-15832.
15. Durham W.B., Goetze C., Blake B. Plastic flow of oriented single crystals of olivine: 2. Observations and interpretations of the dislocations structures. J. Geophys. Res. 82:1977;5755-5770.
16. Durham, W.B., Rubie, D.C., 1998. Can the multianvil apparatus really be used for high-pressure deformation experiments? In: Manghanani, M.H., Yagi, T. (Eds.), Properties of Earth and Planetary Materials at High Pressure and Temperature, Geophysical Monograph 101. Am. Geophys. Union, Washington, DC, pp. 63-70.
17. Edington, J.W., 1976. Practical Electron Microscopy in Materials Science. Philips, Eindhoven, 344 pp.
18. 4, 0.00≤x≤0.40. Phys. Chem. Minerals. 19:1993;361-368.
19. 4. In: Syono, Y., Manghnani, M.H. (Eds.), High Pressure Research: Application to Earth and Planetary Sciences. Terrapub, Tokyo-Am. Geophys. Union., Washington, DC, pp. 237-243.
20. Goto K., Suzuki Z., Hamaguchi H. Stress distribution due to the olivine-spinel phase transition in descending plate and deep focus earthquakes. J. Geophys. Res. 92:1987;13811-13820.
21. Green H.W., Burnley P.C. A new self-organizing mechanism for deep focus earthquakes. Nature. 341:1989;733-737.
22. Green, H.W., Burnley, P.C., 1990. The failure mechanism for deep-focus earthquakes. In: Knipe, R.J., Rutter, E.H. (Eds.), Deformation Mechanisms, Rheology and Tectonics. Geol. Soc. Special Publication, Vol. 54, pp. 133-141.
23. Green H.W., Zhou Y. Transformation-induced faulting requires an exothermic reaction and explains the cessation of earthquakes at the base of the mantle transition zone. Tectonophysics. 256:1996;39-56.
24. Green H.W., Young T.E., Walker D., Scholtz C.H. Anticrack associated faulting at very high pressure in natural olivine. Nature. 348:1990;720-722.
25. Green, H.W., Young, T.E., Walker, D., Sholtz, C.H., 1992. The effect of nonhydrostatic stress on the α→β and α→γ olivine phase transformations. In: Syono, Y., Manghani, M.H. (Eds.), High Pressure Research: Application to Earth and Planetary Sciences. Terrapub, Tokyo-Am. Geophys. Union., Washington, DC, pp. 229-235.
26. Gueguen Y., Darot M. Les dislocations dans la forstérite déformée à haute température. Philos. Mag. A. 45:1982;419-442.
27. 4. Geophys. Res. Lett. 18:1991;89-92.
28. Hazen R.M., Downs R.T., Finger H.W., Ko J. Crystal chemistry of ferromagnesian silicate spinels: Evidence for Mg-Si disorder. Am. Mineral. 78:1993;1320-1323.
29. Hyde B.G., White T.J., O'Keeffe M., Johnson A.W.S. Structures related to those of spinel and the wadsleyite, and a possible mechanism for the transformation olivine-spinel. Z. Krist. 160:1982;53-62.
30. Ito, E., Sato, H., 1992. Effect of phase transformations on the dynamics of the descending slab. In: Syono, Y. Manghnani, M.H. (Eds.), High Pressure Research: Application to Earth and Planetary Sciences. Terrapub, Tokyo-Am. Geophys. Union., Washington, DC, pp. 257-262.
31. Karato, S.I., 1997. Phase transformations and the rheological properties of mantle minerals. In: Crossley, D., Soward, A.M. (Eds.), Earth's Deep Interior (Doornbos Memorial Volume). Gordon & Breach, New York, pp. 223-271.
32. Karato S.I., Rubie D.C. Toward an experimental study of deep mantle rheology: a new multianvil sample assembly for deformation studies under high pressures and temperatures. J. Geophys. Res. 102:1997;20111-20122.
33. Karato S.I., Rubie D.C., Yan H. Dislocation recovery in olivine under deep upper mantle conditions: implications for creep and diffusion. J. Geophys. Res. 98:1993;9761-9768.
34. 4 at high pressures and temperatures: precise determination of stabilities of olivine, modified spinel, and spinel. J. Geophys. Res. 94:1989;15663-15670.
35. Kerschhofer L., Sharp T.G., Rubie D.C. Intracrystalline transformation of olivine to wadsleyite and ringwoodite under subduction zone conditions. Science. 274:1996;79-81.
36. Kerschhofer, L., Dupas, C., Liu, M., Sharp, T.G., Durham, W.B., Rubie, D.C., 1998a. Polymorphic transformations between olivine, wadsleyite and ringwoodite: mechanisms of intracrystalline nucleation and the role of elastic strain. Mineral Mag., in press.
37. Kerschhofer, L., Liu, M., Rubie, D.C., McConnell, J.D.C., Sharp, T.G., Dupas, C., 1998b. Intracrystalline olivine-ringwoodite transformation and time-dependent growth rates. The Proceedings of Joint AIRAPT-16 and HPCJ-38, The Review of High Pressure Science and Technology v. 7, in press.
38. Kirby S.H. Localised polymorphic phase transformations in high-pressure faults and applications to the physical mechanism of deep earthquakes. J. Geophys. Res. 92:1987;13789-13800.
39. Kirby S.H., Durham W.B., Stern L.A. Mantle phase changes and deep earthquake faulting in subducting lithosphere. Science. 252:1991;216-225.
40. Kirby S.H., Stein S., Okal E.A., Rubie D.C. Metastable mantle phase transformations and deep earthquakes in subducting oceanic lithosphere. Rev. Geophys. 34:1996;261-306.
41. Liebermann, R.C., Wang, Y., 1992. Characterization of sample environment in a uniaxial split-sphere apparatus. In: Syono, Y., Manghnani, M.H. (Eds.), High-Pressure Research: Application to Earth and Planetary Sciences. Geophys. Monogr. Ser., Vol. 67. Terra Scientific, Tokyo/AGU, Washington D.C., pp. 19-31.
42. Liu M., Yund R.A. Transformation kinetics of polycrystalline aragonite to calcite: new experimental data, modelling and implications. Contrib. Mineral. Petrol. 114:1993;465-478.
43. 4 in shocked meteorites: planar defects and polymorphic transitions. Phys. Earth Planet. Int. 33:1983;31-44.
44. 3 perovskite-(Mg, Fe)O magnesiowüstite assemblages: an analytical transmission electron microscopy study. J. Geophys. Res. 102:1997;5265-5280.
45. Nord, G.L., Heuer, A.H., Lally, J.S., 1976. Pigeonite exsolution from augite. In: Wenk, H.R. (Ed.), Electron Microscopy in Mineralogy. Springer-Verlag, Berlin, 220-227.
46. 3+ content. Am. Mineral. 78:1993;456-460.
47. Phakey, P., Dollinger, G., Christie, J., 1972. Transmission electron microscopy of experimental deformed olivine crystals. In: Heard, H.C., Borg, I.Y., Carter, N.L., Raleigh, C.B. (Eds.), Flow and Fracture of Rocks. Am. Geophys. Union., Washington, DC, 20036, pp. 117-138.
48. 4 from the Peace River meteorite. Phys. Earth Planet. Int. 33:1983;137-147.
49. 4. Nature. 296:1982;729-731.
50. Raleigh C.B. Mechanisms of plastic deformation of olivine. J. Geophys. Res. 73:1968;5391-5406.
51. 4. Phys. Chem. Minerals. 15:1988;498-506.
52. 4-olivine: a Raman spectroscopic study. Phys. Chem. Minerals. 20:1994;556-562.
53. 4: insights into its high temperature thermodynamic properties and the α to wadsleyite-transformation mechanism and kinetics. Am. Mineral. 81:1996;585-594.
54. Riedel M.R., Karato S.I. Grain size evolution in subducted oceanic lithosphere associated with the olivine-spinel transformation and its effect on rheology. Earth Planet. Sci. Lett. 148:1997;27-44.
55. Rubie D.C. The olivine→spinel transformation and the rheology of subducting lithosphere. Nature. 308:1984;505-508.
56. Rubie, D.C., 1993. Mechanism and kinetics of reconstructive phase transformations in the earth's mantle. In: Luth, R.W. (Ed.), Short Course on Experiments at High Pressure and Applications to the Earth's Mantle, Vol. 21. Mineralogical Association of Canada, Edmonton, pp. 247-303.
57. 4 at high temperature and pressure. Nature. 348:1990;628-631.
58. 4 in the Earth's mantle: mechanisms and rheological implications. Science. 264:1994;1445-1448.
59. Rubie D.C., Ross C.R. II Kinetics of the olivine-spinel transformation in subducting lithosphere: experimental constraints and implications for deep slab processes. Phys. Earth Planet. Int. 86:1994;223-241.
60. Sharp T.G., Rubie D.C. Catalysis of the olivine to spinel transformation by high clinoenstatite. Science. 269:1995;1095-1098.
61. 4 experimentally deformed at transition-zone conditions. Phys. Earth Planet. Int. 86:1994;69-83.
62. Sung C.M., Burns R.G. Kinetics of high pressure phase transformations: implications to the evolution of the olivine→spinel transition in the downgoing lithosphere and its consequences on the dynamics of the mantle. Tectonophysics. 31:1976;1-32.
63. Thompson, J.B., 1981. Polytypism in complex crystals: contrast between mica and classical polytypes. In: O'Keeffe, M., Navrotsky, A. (Eds.), Structure and Bonding in Crystals, Vol. II. Academic Press, New York, pp. 167-196.
64. 4 and its implications for the mechanism of deep focus earthquakes. J. Struct. Geol. 15:1993;1249-1256.
65. Turnbull D. Phase changes. Solid State Phys. 3:1956;225-306.
66. Van Cappellen E. The parameterless correction method in X-ray microanalysis. Microsc. Microanal. Microstruct. 1:1990;1-22.
67. Van Cappellen E., Doukhan J.C. Quantitative transmission X-ray microanalysis of ionic compounds. Ultramicroscopy. 53:1994;343-349.
68. 4 under non hydrostatic stress. Tectonophysics. 108:1984;299-322.
69. 4 and the mechanism of deep earthquakes. J. Geophys. Res. 98:1993;19767-19776.
70. Zeuch D.H., Green H.W. Experimental deformation of a synthetic dunite at high temperature and pressure: Part II. Transmission electron microscopy. Tectonophysics. 110:1984;263-296.