High pressure equations of state with applications to the lower mantle and core
By F. Stacey, P. Davis. 2004
237 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/a2837956a8d9723a95969f37182d72d70da81c4e
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In Geophysics
Citations in the corpus
- Solidus and liquidus profiles of chondritic mantle: Implication for melting of the Earth across its history (2011, background): “Differences in adiabatic geotherms are often within 0.1 K/km but translate into up to 250 K difference at the bottom of the mantle yielding in general 2500 K±250 at 2700 km depth (Brown and Shankland, 1981; Bunge et al., 2001; Stacey and Davis, 2004).”