Energetics of mantle convection and the fate of fossil heat

By Jun Korenaga. 2003

157 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/99fa171cf2af747eb8d31fb578e92e0dbae6254c

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In Geophysics

Citations in the corpus

Archean Geodynamics and the Thermal Evolution of Earth (2013, background): “Thus, when only thermal effects are considered, plate-tectonic convection behaves like classical thermal convection even with this extra dissipation [Korenaga, 2003].”
Urey ratio and the structure and evolution of Earth's mantle (2008, background): “…and heat loss, and if convective heat loss is maintained at a relatively uniform level as suggested by some recent heat flow scaling laws [e.g., Solomatov, 2001; Korenaga, 2003], the average rate of secular cooling since the Archean may be reduced to 50–100 K Ga 1 (see Figure 5a and section 3.4).”
Energetics of the Core (2015, background): “Secondly, the effect of mantle temperature on plate tectonic behaviour is not well understood, with even the sign of the effect being disputed (e.g. Korenaga 2003); similarly, the change in mean plate tectonic velocities over billions of years is unknown.”
Temperatures, Heat, and Energy in the Mantle of the Earth (2007, methodology): “Lyubetskaya and Korenaga (2007) have recently revisited the procedure of McDonough and Sun (1995).”
Evolution of U-Pb and Sm-Nd systems in numerical models of mantle convection and plate tectonics (2004, background): “The total surface heat flow (plotted using a 500 Myr running average to emphasize the long-term trend) decreases from about 100 TW to 20 TW over the course of the calculation, the present value being lower than the estimated mantle heat flow of 34 TW, a perennial problem in mantle thermal evolution ”
Thermal cracking and the deep hydration of oceanic lithosphere: A key to the generation of plate tectonics? (2007, background): “Citation: Korenaga, J. (2007), Thermal cracking and the deep hydration of oceanic lithosphere: A key to the generation of plate”
Rheology of the Earth's mantle: A historical review (2010, background): “In this context, Korenaga (2007) suggested that thermal cracking could transfer water down to∼20 km depth of the oceanic lithosphere.”
Thermal history of the Earth and its petrological expression (2010, methodology): “The scaling of Korenaga (2003) thus does not require extreme conditions as Davies (2009) argued.”
LINKS BETWEEN LONG‐LIVED HOT SPOTS, MANTLE PLUMES, D″, AND PLATE TECTONICS (2004, background): “Moreover, viscosity varies by at most a factor of 5–10 across the active or convecting part of the cold thermal boundary layer [e.g., Richter et al., 1983; Davaille and Jaupart, 1993; Deschamps and Sotin, 2000; Korenaga and Jordan, 2003].”