Whether convection in the Earth's mantle extends through its entire depth or if the mantle is layered has long been debated. Recent research suggests that spatially and temporally intermittent or partial layering is the most likely solution.
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References
Hofmann, A. W. in Treatise on Geochemistry (ed. Carlson, R. W.) 61–101 (Elsevier, Amsterdam, 2003).
Fukao, Y., Obayashi, M., Inoue, H. & Nenbai, M. J. Geophys. Res. 97, 4809–4822 (1992).
Grand, S. P. Phil. Trans. R. Soc. Lond. A 360, 2475–2491 (2002).
Schubert, G., Turcotte, D. L. & Olson, P. Mantle Convection in the Earth and Planets (Cambridge Univ. Press, Cambridge, 2000).
Tackley, P. J. in Treatise on Geophysics Vol. 7: Mantle Dynamics (eds Bercovici D. & Schubert, G.) 437–505 (Elsevier, Amsterdam, 2007).
Trampert, J., Deschamps, F., Resovsky, J. S. & Yuen, D. A. Science 306, 853–856 (2004)
Ishii, M. & Tromp, J. Science 285, 1231–1235 (1999).
Bizimis, M., Griselin, M., Lassiter, J. C. Salters, V. J. M. & Sen, G. Earth Plan. Sci. Lett. 257, 259–293 (2007).
Bercovici, D. & Karato, S. Nature 425, 39–44 (2003).
Labrosse, S., Hernlund J. & Coltice, N. Nature 450, 866–869 (2007).
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Tackley, P. Layer cake or plum pudding?. Nature Geosci 1, 157–158 (2008). https://doi.org/10.1038/ngeo134
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DOI: https://doi.org/10.1038/ngeo134
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