Embryos of TTGs in Gore Mountain garnet megacrysts from water-fluxed melting of the lower crust
Autor: | Robert Darling, Oscar Laurent, Iris Wannhoff, Patrick J. O'Brien, Alessia Borghini, Silvio Ferrero, Bernd Wunder, Chris Yakymchuk |
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Přispěvatelé: | Géosciences Environnement Toulouse (GET), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS) |
Jazyk: | angličtina |
Rok vydání: | 2021 |
Předmět: |
010504 meteorology & atmospheric sciences
Subduction Gabbro Continental crust Partial melting [SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography [SDU.STU]Sciences of the Universe [physics]/Earth Sciences Crust 010502 geochemistry & geophysics 01 natural sciences Geophysics 13. Climate action Space and Planetary Science Geochemistry and Petrology [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry Earth and Planetary Sciences (miscellaneous) [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology Mafic Petrology Geology ComputingMilieux_MISCELLANEOUS 0105 earth and related environmental sciences Melt inclusions Terrane |
Zdroj: | Earth and Planetary Science Letters Earth and Planetary Science Letters, Elsevier, 2021, 569, pp.117058. ⟨10.1016/j.epsl.2021.117058⟩ BASE-Bielefeld Academic Search Engine Earth and Planetary Science Letters, 2021, 569, pp.117058. ⟨10.1016/j.epsl.2021.117058⟩ |
ISSN: | 0012-821X |
DOI: | 10.1016/j.epsl.2021.117058⟩ |
Popis: | The garnet megacrysts of Gore Mountain (Adirondacks, US) are world-renown crystals due to their size, up to 1 m in historical record, which makes them the largest known garnets on the planet. We show here that they are also host to the first primary inclusions of trondhjemitic melt found in natural mafic rocks. The petrological and experimental investigation of the inclusions, coupled with phase equilibrium modelling, shows that this melt is the result of H2O-fluxed partial melting at T > 900 °C of a lower crustal gabbro. The compositional similarity between the trondhjemitic melt inclusions and tonalitic–trondhjemitic–granodioritic (TTGs) melts makes these inclusions a direct natural evidence that melting of mafic rocks generates TTG-like melts, and provides us with the possibility to clarify processes responsible for the formation of the early continental crust. These TTG embryos represent the trondhjemitic end-member of the melts whose emplacement at upper crustal levels, after being modified by mixing and crystallization-related processes, leads to the formation of the TTG terranes. Moreover, our study shows how the melt from H2O-fluxed melting of mafic lower crust has mismatched major and trace element signatures, previously interpreted as evidence of melting at very different pressures. This poses serious limitations to the established use of some chemical features to identify the geodynamic settings (e.g. subduction versus thickened crust) responsible for TTGs generation and the growth of early crust. |
Databáze: | OpenAIRE |
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