Deformation-induced grain boundary wetting and its effects on the acoustic and rheological properties of partially molten rock analogue

Journal of Geophysical Research: Solid Earth

Volumn 110, Issue 12, 2005, Pages 1-24

  Takei, Yasuko ^a  

^a UNIVERSITY OF TOKYO   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

ACOUSTIC PROPERTY; GRAIN BOUNDARY; IGNEOUS GEOCHEMISTRY; PARTIAL MELTING; RHEOLOGY; WETTING;

EID: 31544437165     PISSN: 21699313     EISSN: 21699356     Source Type: Journal    
DOI: 10.1029/2005JB003801     Document Type: Article

References (42)

1. Bai, Q., Z.-M. Jin, and H. W. Green (1997), Experimental investigation of the rheology of partially molten peridotite at upper mantle pressures and temperatures, in Deformation-Enhanced Fluid Transport in the Earth's Crust and Mantle, edited by M. B. Holness, pp. 40-61, CRC Press, Boca Raton, Fla.
2. Cooper, R. F., and D. L. Kohlstedt (1986), Rheology and structure of olivine-basalt partial melts, J. Geophys. Res., 91, 9315-9323.
3. Daines, M. J., and D. L. Kohlstedt (1997), Influence of deformation on melt topology in peridotites, J. Geophys. Res., 102, 10,257-10,271.
4. Hier-Majumder, S., P. H. Leo, and D. L. Kohlstedt (2004), On grain boundary wetting during deformation, Acta Mater., 52, 3425-3433.
5. Hirth, G., and D. L. Kohlstedt (1995a), Experimental constraints on the dynamics of the partially molten upper mantle: Deformation in the diffusion creep regime, J. Geophys. Res., 100, 1981-2001.
6. Hirth, G., and D. L. Kohlstedt (1995b), Experimental constraints on the dynamics of the partially molten upper mantle. 2: Deformation in the dislocation creep regime, J. Geophys. Res., 100, 15,441-15,449.
7. 2O on the permeability of quartzites, Earth Planet. Sci. Lett., 117, 363-377.
8. Holness, M. B. (1997), Surface chemical controls on pore-fluid connectivity in texturally equilibrated materials, in Fluid Flow and Transport in Rocks, edited by B. Jamtveit and M. Yardley, pp. 149-169, CRC Press, Boca Raton, Fla.
9. Holtzman, B. K., N. J. Groebner, M. E. Zimmerman, S. B. Ginsberg, and D. L. Kohlstedt (2003a), Stress-driven melt segregation in partially molten rocks, Geochem. Geophys. Geosyst., 4(5), 8607, doi:10.1029/2001GC000258.
10. Holtzman, B. K., D. L. Kohlstedt, M. E. Zimmerman, F. Heidelbach, T. Hiraga, and J. Hustoft (2003b), Melt segregation and strain partitioning: Implications for seismic anisotropy and mantle flow, Science, 301, 1227-1230.
11. Jackson, I., J. D. Fitz Gerald, U. H. Faul, and B. H. Tan (2002), Grain-size-sensitive seismic wave attenuation in polycrystalline olivine, J. Geophys. Res., 107(B12), 2360, doi:10.1029/2001JB001225.
12. Jackson, I., U. H. Faul, J. D. Fitz Gerald, and B. H. Tan (2004), Shear wave attenuation and dispersion in melt-bearing olivine polycrystals: 1. Specimen fabrication and mechanical testing, J. Geophys. Res., 109, B06201, doi:10.1029/2003JB002406.
13. Jin, Z. M., H. W. Green, and Y. Zhou (1994), Melt topology in partially molten mantle peridotite during ductile deformation, Nature, 372, 164-167.
14. Karato, S. (1993), Importance of anelasticity in the interpretation of seismic tomography, Geophys. Res. Lett., 20, 1623-1626.
15. Lehner, F. K. (1995), A model for intergranular pressure solution in open systems, Tectonophysics, 245, 153-170.
16. Mavko, G. M. (1980), Velocity and attenuation in partially molten rocks, J. Geophys. Res., 85, 5173-5189.
17. Mei, S., W. Bai, T. Hiraga, and D. L. Kohlstedt (2002), Influence of melt on the creep behavior of olivine-basalt aggregates under hydrous conditions, Earth Planet. Sci. Lett., 201, 491-507.
18. Nakajima, J., and A. Hasegawa (2004), Shear-wave polarization anisotropy and subduction-induced flow in the mantle wedge of northeastern Japan, Earth Planet. Sci. Lett., 225, 365-377.
19. s beneath northeastern Japan: Implications for arc magmatism and fluids, J. Geophys. Res., 106, 21,843-21,857.
20. Nakajima, J., Y. Takei, and A. Hasegawa (2005), Quantitative analysis of the inclined low-velocity zone in the mantle wedge of northeastern Japan: A systematic change of melt-filled pore shapes with depth and its implications for melt migration, Earth Planet. Sci. Lett., 234, 59-70.
21. Nowick, A. S., and B. S. Berry (1972), Anelastic Relaxation in Crystalline Solids, Elsevier, New York.
22. O'Connell, R. J., and B. Budiansky (1974), Seismic velocities in dry and saturated cracked solids, J. Geophys. Res., 79, 5412-5426.
23. Raj, R. (1986), Unstable spreading of a fluid inclusion in a grain boundary under normal stress, J. Am. Ceram. Soc., 69, 708-712.
24. Raj, R., and M. F. Ashby (1971), On grain boundary sliding and diffusional creep, Metall. Trans., 2, 1113-1127.
25. Sherwood, J. N. (1979), Lattice defects, self-diffusion, and the plasticity of plastic crystals, in The Plastically Crystalline State, edited by J. N. Sherwood, pp. 39-83, Wiley-Interscience, Hoboken, N. J.
26. Stevenson, D. J. (1986), On the role of surface tension in the migration of melts and fluids, Geophys. Res. Lett., 13, 1149-1152.
27. Takei, Y. (1998), Constitutive mechanical relations of solid-liquid composites in terms of grain-boundary contiguity, J. Geophys. Res., 103, 18,183-18,203.
28. Takei, Y. (2000), Acoustic properties of partially molten media studied on a simple binary system with a controllable dihedral angle, J. Geophys. Res., 105, 16,665-16,682.
29. Takei, Y. (2001), Stress-induced anisotropy of partially molten media inferred from experimental deformation of a simple binary system under acoustic monitoring, J. Geophys. Res., 106, 567-588.
30. s: From equilibrium geometry to crack, J. Geophys. Res., 107(B2), 2043, doi:10.1029/2001JB000522.
31. Toramaru, A., and N. Fujii (1986), Connectivity of melt phase in a partially molten peridotite, J. Geophys. Res., 91, 9239-9252.
32. Urai, J. L. (1983), Water assisted dynamic recrystallization and weakening in polycrystalline bischofite, Tectonophysics, 96, 125-157.
33. Urai, J. L., C. J. Spiers, H. J. Zwart, and G. S. Lister (1986), Weakening of rock salt by water during long-term creep, Nature, 324, 554-557.
34. von Bargen, N., and H. S. Waff (1986), Permeabilities, interfacial areas and curvatures of partially molten systems: Results of computations of equilibrium microstructures, J. Geophys. Res., 91, 9261-9276.
35. Waff, H. S., and J. R. Bulau (1979), Equilibrium fluid distribution in an ultramafic partial melt under hydrostatic stress conditions, J. Geophys. Res., 84, 6109-6114.
36. Waff, H. S., and U. H. Faul (1992), Effects of crystalline anisotropy on fluid distribution in ultramafic partial melts, J. Geophys. Res., 97, 9003-9014.
37. Watson, E. B. (1999), Lithologic partitioning of fluids and melts, Am. Mineral., 84, 1693-1710.
38. 2O fluids and their implications for fluid transport, host-rock physical properties, and fluid inclusion formation, Earth Planet. Sci. Lett., 85, 497-515.
39. Wark, D. A., C. A. Williams, E. B. Watson, and J. D. Price (2003), Reassessment of pore shapes in microstructurally equilibrated rocks, with implications for permeability of the upper mantle, J. Geophys. Res., 108(B1), 2050, doi:10.1029/2001JB001575.
40. Yamamura, K., O. Sano, H. Utada, Y. Takei, S. Nakao, and Y. Fukao (2003), Long-term observation of in situ seismic velocity and attenuation, J. Geophys. Res., 108(B6), 2317, doi:10.1029/2002JB002005.
41. Yoshino, T., Y. Takei, D. A. Wark, and E. B. Watson (2005), Grain boundary wetness of texturally equilibrated rocks, with implications for seismic properties of the upper mantle, J. Geophys. Res., 110, B08205, doi:10.1029/2004JB003544.
42. Zimmerman, M. E., and D. L. Kohlstedt (2004), Rheological properties of partially molten Lherzolite, J. Petrol., 45, 275-298.