Thermal history of the Earth and its petrological expression

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Primary magmas and mantle temperatures through time (2017, methodology): “In their model, all Precambrian rocks may be interpreted as the melting products of the ambient mantle [Herzberg et al., 2010], which is considered as thermally heterogeneous, mostly hot but with some colder exceptions [Herzberg, 2016].”
Geophysics of Chemical Heterogeneity in the Mantle (2012, background): “F or p er so na l u se o nl y. EA40CH23-Stixrude ARI 1 April 2012 8:42 in agreement with evidence from ancient lavas (Herzberg et al. 2010).”
Crustal evolution and the temporality of anorthosites (2017, background): “…it has been suggested that the Neoarchean-Paleoproterozoic boundary marks the transition from a planet where internal heating (via radioactive decay) exceeds surface heat loss (via mantle convection), to one in which a secular cooling mode dominates (Herzberg et al., 2010; Korenaga 2008).”
Processes on the Young Earth and the Habitats of Early Life (2012, background): “From Herzberg et al. (2010). www.annualreviews.org • Habitats of Early Life 525 A nn u.”