Effects of Partial Melting on Seismic Velocity and Attenuation: A New Insight from Experiments

Literature Cited

1. Aki K, Richards PG. 2002. Quantitative Seismology Sausalito, CA: Univ. Sci. Books
2. Anderson DL. 1989. Theory of the Earth Boston: Blackwell Sci.
3. Bass JD. 1995. Elasticity of minerals, glasses and melts. Mineral Physics and Crystallography TJ Ahrens 45–63 Washington, DC: Am. Geophys. Union [Google Scholar]
4. Cantwell PR, Tang M, Dillon SJ, Luo J, Rohrer GS, Harmer MP. 2014. Grain boundary complexions. Acta Mater. 62:1–48 [Google Scholar]
5. Cooper RF. 2002. Seismic wave attenuation; energy dissipation in viscoelastic crystalline solids. Rev. Mineral. Geochem. 51:1253–90 [Google Scholar]
6. Dalton CA, Ekström G, Dziewonski AM. 2009. Global seismological shear velocity and attenuation: a comparison with experimental observations. Earth Planet. Sci. Lett. 284:65–75 [Google Scholar]
7. Dasgupta R, Hirschmann MM, Smith ND. 2007. Water follows carbon: CO₂ incites deep silicate melting and dehydration beneath mid-ocean ridges. Geology 35:135–38 [Google Scholar]
8. Faul UH, Jackson I. 2005. The seismological signature of temperature and grain size variations in the upper mantle. Earth Planet. Sci. Lett. 234:119–34 [Google Scholar]
9. Faul UH, Jackson I. 2007. Diffusion creep of dry, melt-free olivine. J. Geophys. Res. 112:B04204 [Google Scholar]
10. Gribb TT, Cooper RF. 1998. Low-frequency shear attenuation in polycrystalline olivine: grain boundary diffusion and the physical significance of the Andrade model for viscoelastic rheology. J. Geophys. Res. 103:B1127267–79 [Google Scholar]
11. Hiraga T, Anderson IM, Zimmerman ME, Mei S, Kohlstedt DL. 2002. Structure and chemistry of grain boundaries in deformed, olivine+basalt and partially molten lherzolite aggregates: evidence of melt-free grain boundaries. Contrib. Mineral. Petrol. 144:163–75 [Google Scholar]
12. Hirschmann MM. 2000. Mantle solidus: experimental constraints and the effects of peridotite composition. Geochem. Geophys. Geosyst. 1:1042 [Google Scholar]
13. Hirschmann MM. 2010. Partial melt in the oceanic low velocity zone. Phys. Earth Planet. Inter. 179:60–71 [Google Scholar]
14. Hirth G, Kohlstedt DL. 1996. Water in the oceanic upper mantle: implications for rheology, melt extraction and the evolution of the lithosphere. Earth Planet. Sci. Lett. 144:93–108 [Google Scholar]
15. Hirth G, Kohlstedt DL. 2003. Rheology of the upper mantle and the mantle wedge: a view from the experimentalists. Geophys. Monogr. Ser. 138:83–105 [Google Scholar]
16. Isaak DG. 1992. High-temperature elasticity of iron-bearing olivines. J. Geophys. Res. 97:B21871–85 [Google Scholar]
17. Jackson I, Faul UH. 2010. Grainsize-sensitive viscoelastic relaxation in olivine: towards a robust laboratory-based model for seismological application. Phys. Earth Planet. Inter. 183:151–63 [Google Scholar]
18. Jackson I, Faul UH, Fitz Gerald JD, Tan BH. 2004. Shear wave attenuation and dispersion in melt-bearing olivine polycrystals: 1. Specimen fabrication and mechanical testing. J. Geophys. Res. 109:B06201 [Google Scholar]
19. Jackson I, Fitz Gerald JD, Faul UH, Tan BH. 2002. Grain-size-sensitive wave attenuation in polycrystalline olivine. J. Geophys. Res. 107:B122360 [Google Scholar]
20. Karato S. 1993. Importance of anelasticity in the interpretation of seismic tomography. Geophys. Res. Lett. 20:1623–26 [Google Scholar]
21. Lee LC, Morris SJS, Wilkening J. 2011. Stress concentrations, diffusionally accommodated grain boundary sliding and the viscoelasticity of polycrystals. Proc. R. Soc. A 467:1624–44 [Google Scholar]
22. Mavko GM. 1980. Velocity and attenuation in partially molten rocks. J. Geophys. Res. 85:5173–89 [Google Scholar]
23. McCarthy C, Takei Y. 2011. Anelasticity and viscosity of partially molten rock analogue: toward seismic detection of small quantities of melt. Geophys. Res. Lett. 38:L18306 [Google Scholar]
24. McCarthy C, Takei Y, Hiraga T. 2011. Experimental study of attenuation and dispersion over a broad frequency range: 2. The universal scaling of polycrystalline materials. J. Geophys. Res. 116:B09207 [Google Scholar]
25. McKenzie D. 1985. The extraction of magma from the crust and mantle. Earth Planet. Sci. Lett. 74:81–91 [Google Scholar]
26. McKenzie D. 2000. Constraints on melt generation and transport from U-series activity ratios. Chem. Geol. 162:81–94 [Google Scholar]
27. McKenzie D, Bickle MJ. 1988. The volume and composition of melt generated by extension of the lithosphere. J. Petrol. 29:3625–79 [Google Scholar]
28. McKenzie D, Jackson J, Priestley K. 2005. Thermal structure of oceanic and continental lithosphere. Earth Planet. Sci. Lett. 233:337–49 [Google Scholar]
29. Morris SJS, Jackson I. 2009. Diffusionally assisted grain-boundary sliding and viscoelasticity of polycrystals. J. Mech. Phys. Solids 57:744–61 [Google Scholar]
30. Nowick AS, Berry BS. 1972. Anelastic Relaxation in Crystalline Solids San Diego, CA: Academic
31. O'Connell RJ, Budiansky B. 1974. Seismic velocities in dry and saturated cracked solids. J. Geophys. Res. 79:5412–26 [Google Scholar]
32. O'Connell RJ, Budiansky B. 1978. Measures of dissipation in viscoelastic media. Geophys. Res. Lett. 5:5–8 [Google Scholar]
33. Priestley K, McKenzie D. 2006. The thermal structure of the lithosphere from shear wave velocities. Earth Planet. Sci. Lett. 244:285–301 [Google Scholar]
34. Priestley K, McKenzie D. 2013. The relationship between shear wave velocity, temperature, attenuation and viscosity in the shallow part of the mantle. Earth Planet. Sci. Lett. 381:78–91 [Google Scholar]
35. Raj R. 1975. Transient behavior of diffusion-induced creep and creep rupture. Metall. Mater. Trans. A 6:1499–509 [Google Scholar]
36. Raj R, Ashby MF. 1971. On grain boundary sliding and diffusional creep. Metall. Mater. Trans. B 2:1113–27 [Google Scholar]
37. Rudge J. 2016. The rheology of the partially molten mantle. Presented at Symp. Study Earth's Deep Inter., 15th, July 24–29, Nantes, Fr. https://sedi2016.sciencesconf.org/conference/sedi2016/pages/SEDI2016_AbstractBookv2.pdf
38. Stixrude L, Lithgow-Bertelloni C. 2005. Mineralogy and elasticity of the oceanic upper mantle: origin of the low-velocity zone. J. Geophys. Res. 110:B03204 [Google Scholar]
39. Takei Y. 1998. Constitutive mechanical relations of solid-liquid composites in terms of grain-boundary contiguity. J. Geophys. Res. 103:B818183–203 [Google Scholar]
40. Takei Y. 2002. Effect of pore geometry on V_P/V_S: from equilibrium geometry to crack. J. Geophys. Res. 107:B22043 [Google Scholar]
41. Takei Y, Holtzman BK. 2009. Viscous constitutive relations of solid-liquid composites in terms of grain boundary contiguity: 1. Grain boundary diffusion control model. J. Geophys. Res. 114:B06205 [Google Scholar]
42. Takei Y, Karasawa F, Yamauchi H. 2014. Temperature, grain size, and chemical controls on polycrystal anelasticity over a broad frequency range extending into the seismic range. J. Geophys. Res. Solid Earth 119:5414–43 [Google Scholar]
43. Tan BH, Jackson I, Fitz Gerald JD. 2001. High-temperature viscoelasticity of fine-grained polycrystalline olivine. Phys. Chem. Miner. 28:641–64 [Google Scholar]
44. Tang M, Carter WC, Cannon RM. 2006. Grain boundary transitions in binary alloys. Phys. Rev. Lett. 97:075502 [Google Scholar]
45. Yamauchi H, Takei Y. 2016. Polycrystal anelasticity at near-solidus temperatures. J. Geophys. Res. Solid Earth 121:7790–820 [Google Scholar]
46. Zhao S, Lambeck K, Lidberg M. 2012. Lithosphere thickness and mantle viscosity inverted from GPS-derived deformation rates in Fennoscandia. Geophys. J. Int. 190:278–92 [Google Scholar]