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- W3000593750 endingPage "105615" @default.
- W3000593750 startingPage "105615" @default.
- W3000593750 abstract "Abstract Different geodynamic models exist for the growth and differentiation of Archean continental crust, ranging from horizontal tectonics with subduction zones to vertical tectonics with foundering of greenstone sequences. U–Pb zircon geochronology, field relationships, and pressure–temperature constraints from granulite-facies metabasite of the Akia Terrane of the North Atlantic Craton in West Greenland show that this terrane grew through two major magmatic growth episodes: an earlier one at c. 3.2 Ga, and a later one at c. 3.05–2.97 Ga. Phase equilibrium modelling for assemblages related to the latter indicates temperatures of >800 °C at 0.8 GPa in the stability field of garnet. U–Pb zircon geochronology and existing Hf isotope data are also consistent with a model involving protracted Mesoarchean magmatic growth with limited mantle addition during a prolonged period of high temperatures in a relatively stagnant tectonic regime prior to Neoarchean compressional tectonism in the Akia Terrane." @default.
- W3000593750 created "2020-01-23" @default.
- W3000593750 creator A5001089827 @default.
- W3000593750 creator A5013096034 @default.
- W3000593750 creator A5017879395 @default.
- W3000593750 creator A5067508584 @default.
- W3000593750 creator A5084730478 @default.
- W3000593750 creator A5091138046 @default.
- W3000593750 date "2020-04-01" @default.
- W3000593750 modified "2023-10-03" @default.
- W3000593750 title "Mesoarchean partial melting of mafic crust and tonalite production during high-T–low-P stagnant tectonism, Akia Terrane, West Greenland" @default.
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