Eoarchean contrasting ultra-high-pressure to low-pressure metamorphisms (<250 to >1000 °C/GPa) explained by tectonic plate convergence in deep time
Allen P. Nutman, Vickie C. Bennett, C. R. L. Friend, Keewook Yi
Topics & Concepts
GeologyAnatexisMetamorphismGeochemistryGranulitePartial meltingMaficCrustMetamorphic rockPetrologyFelsicGneissGeomorphologyFaciesStructural basinGeological and Geochemical AnalysisHigh-pressure geophysics and materialsearthquake and tectonic studies