Abstract
EXPERIMENTS on model materials show that the acoustic properties of the low velocity zone (LVZ) can arise from the formation of intergranular fluid or melt with no significant reduction in creep strength. Consequently, only very limited bounds on the asthenosphere can be inferred from seismic data.
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References
Sherby, O. D., and Burke, P. M., Prog. Mater. Sci., 13, 325–390 (1968).
Stocker, R. L., and Ashby, M. F., Rev. Geophys. Space Phys., 11, 391–426 (1973).
Gordon, R. B., J. geophys. Res., 70, 2413–2418 (1965).
Weertman, J., Rev. Geophys. Space Phys., 8, 145–168 (1970).
Nowick, A. S., and Berry, B., Anelastic Relaxation in Crystalline Solids (Academic Press, New York, 1972).
Umekawa, S., Kotfila, R., and Sherby, O. D., J. Mech. Phys. Solids, 13, 229–235 (1965).
Stocker, R. L., thesis, Yale Univ. (1973).
Spetzler, H., and Anderson, D., J. geophys. Res., 73, 6051–6060 (1968).
Goetze, C., thesis, Harvard Univ. (1969).
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AUTEN, T., GORDON, R. & STOCKER, R. Q and mantle creep. Nature 250, 317–318 (1974). https://doi.org/10.1038/250317a0
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DOI: https://doi.org/10.1038/250317a0
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