Original paper
Reconciling thermal regimes and tectonics of the early Earth
Abstract
Thermomechanical models of mantle convection and melting in an inferred hotter Archean Earth show the emergence of pressure-temperature (P-T) regimes that resemble present-day plate tectonic environments yet developed within a non–plate tectonics regime. The models’ P-T gradients are compatible with those inferred from evolving tonalite-trondhjemite-granodiorite series rocks and the paired metamorphic belt record, supporting the feasibility of...
Paper Details
Title
Reconciling thermal regimes and tectonics of the early Earth
Published Date
Aug 20, 2019
Journal
Volume
47
Issue
10
Pages
923 - 927
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Notes
History