Articles | Volume 35, issue 6
https://doi.org/10.5194/ejm-35-1031-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/ejm-35-1031-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
H2O and Cl in deep crustal melts: the message of melt inclusions in metamorphic rocks
Dipartimento di Scienze Chimiche e Geologiche, Università degli Studi di Cagliari, Cittadella Universitaria di Monserrato S.S. 554 Bivio Sestu, 09042 Monserrato, Italy
Alessia Borghini
Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, 30-059 Kraków, Poland
Institute of Geosciences, University of Potsdam, 14476 Potsdam, Germany
Laurent Remusat
Institut de Minéralogie, Physique des Matériaux et Cosmochimie, CNRS UMR 7590, Sorbonne Université, Muséum National d'Histoire Naturelle, CP52, 57 rue Cuvier, 75005 Paris, France
Gautier Nicoli
Yorkshire Peat Partnership, BD23 1UD, Skipton, United Kingdom
Bernd Wunder
Helmholtz-Zentrum Potsdam, GFZ, 14473 Potsdam, Germany
Roberto Braga
Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Università di Bologna, Piazza di Porta S. Donato 1, 40126 Bologna, Italy
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Short summary
Garnet often entraps small droplets of deep melts generated during mountain building processes. Using high-resolution techniques, we studied these droplets in order to provide hard numbers for the quantification of volatile budgets during crustal evolution, show how even melts formed at >1000°C contain water, and clarify how water behaves during metamorphism and melting at the microscale. Moreover, we provide the very first data on chlorine in natural melts from crustal reworking.
Garnet often entraps small droplets of deep melts generated during mountain building processes....