Thermal evolution of the Earth: Secular changes and fluctuations of plate characteristics

By Stéphane Labrosse, Claude Jaupart. 2007

204 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/c202ddcf9ce398139f2f7830b4a0893ea1c92d66

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In Geophysics

Citations in the corpus

Primary magmas and mantle temperatures through time (2017, background): “How this balance has varied over geological time is still under discussion in the light of geophysical modeling of the thermal evolution of the Earth [Korenaga, 2006; Labrosse and Jaupart, 2007; Davies, 2009; Lourenco et al., 2016, and references therein].”
Processes on the Young Earth and the Habitats of Early Life (2012, background): “An alternative view is that accelerated convection resulted in more efficient transfer of heat to the surface and that this transfer buffered internal temperatures to values only slightly greater than those in the modern mantle (Labrosse & Jaupart 2007).”
Subduction styles in the Precambrian: Insight from numerical experiments (2009, background): “On the one hand, there is a variety of evidence for Archean, particularly Mesoarchean-to-Neoarchean, plate tectonics and subduction settings (e.g. de Wit, 1998; Brown, 2006; Condie and Pease, 2008), but some authors argue that modern style subduction only began since the appearance of features such ”
Crustal evolution and the temporality of anorthosites (2017, background): “16a; Herzberg et al., 2010; Korenaga 2008; Labrosse and Jaupart 2007).”
Thermal evolution of the core with a high thermal conductivity (2014, unknown): “Labrosse and Jaupart, 2007; Loyd et al., 2007; Becker et al., 2009; Coltice et al., 2012).”
Thermal history of the Earth and its petrological expression (2010, result): “…of a high Urey ratio due to lower time-averaged surface heat flux (instead of higher internal heat production) was also considered (e.g., Labrosse and Jaupart, 2007), but this notion has been discounted as being inconsistent with the geological record (Korenaga, 2007; Loyd et al., 2007).”
Why is terrestrial subduction one-sided? (2008, background): “…plates are: (1) mantle convection models that explore weak plates are unable to explain the absence of correlation between plate age and subduction (Labrosse and Jaupart, 2007); and (2) the observed plate age distribution requires that the buoyancy of slabs is transmitted to plates by a…”