Mantle Convection in the Earth and Planets [M]. Cambridge Univ Press, New York, 2002.Schubert, G., D. L. Turcotte, and P. Olson, Mantle Convection in the Earth and Planets, Cambridge Univ. Press, Cambridge, 940, 2001.SchubertG,Turcotte D L,Olson P.Mantle Convection in the Earth and...
Mantle Convection in the Earth and Planets (Cambridge University Press, 2001). Herzberg, C., Condie, K. & Korenaga, J. Thermal history of the Earth and its petrological expression. Earth Planet. Sci. Lett. 292, 79–88 (2010). Article CAS Google Scholar Condie, K. C., Aster, R. ...
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Mantle Convection in the Earth and Planets Cambridge University Press, Cambridge (2001) Google Scholar Scotese, 1997 C.R. Scotese Continental Drift Flipbook (7th ed.), PALEOMAP Project, Arlington, Texas (1997) (80 pp.) Google Scholar Scotese, 2004 C.R. Scotese A continental drift flipbook Jou...
Variable viscosity convection experiments with a stress-free upper boundary and implications for the heat transport in the Earth's mantle Physics of the Earth and Planetary InteriorsGiannandrea, E. and U. Christensen, Variable viscosity convec- tion experiments with a stress-free upper ... E Gianna...
Large-scale numerical simulations of two-dimensional thermal convection have been conducted in the strong time-dependent regime for infinite Prandtl number fluids, as applied to the Earth's mantle. Both Newtonian and non-Newtonian (strain-rate proportional to the third power of the deviatoric stress...
Convection Currents and Plate Movements:The Earth, our home planet, is geologically active. The upper layer of the Earth, called the crust, is broken into several pieces, which are constantly moving, giving rise to new land or destroying it. The crust float...
magma ocean solidificationmagma ocean forniationTheory and observations point to the occurrence of magma ponds or oceans in the early evolution of terrestrial... Elkins-Tanton,T Linda - 《Annual Review of Earth & Planetary Sciences》 被引量: 225发表: 2012年 Neon isotopes constrain convection and ...
The pattern and style of mantle convection govern the thermal evolution, internal dynamics, and large-scale surface deformation of the terrestrial planets. In order to characterize the nature of heat transport and convective behaviour at Rayleigh numbers, Ra, appropriate for planetary mantles (between ...
the crust, which is defined at its base by the discontinuity in seismic wave behaviour, as cited above.) They ride on a weak, perhaps partially molten, layer of the upper mantle called theasthenosphere. Slowconvection currentsdeep within the mantle generated by radioactive heating of the ...