Silicic magma petrogenesis in Iceland by remelting of hydrothermally altered crust based on oxygen isotope diversity and disequilibria between zircon and magma with implications for MO
International audience Petrogenesis of silicic magmas in Iceland has fundamental significance for understanding the relative importance of fractional crystallization of mantle-derived basalt and partial melting of hydrothermally altered basaltic crust in formation of the earliest continental crust....
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Bibliographic Details
Published in: | Terra Nova |
Main Authors: |
Bindemand, Ilya,
Gurenko, Andrey,
Camara, Tamara,
Miller, Calvin,
Martin, Erwan,
Sigmarsson, Olgeir |
Other Authors: |
Institut des Sciences de la Terre de Paris (iSTeP),
Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS),
Laboratoire Magmas et Volcans (LMV),
Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet Saint-Étienne (UJM)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC),
Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS),
Institute of Earth Sciences Reykjavik,
University of Iceland Reykjavik |
Format: | Article in Journal/Newspaper
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Language: | English |
Published: |
HAL CCSD
2012
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Subjects: |
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Online Access: | https://hal.archives-ouvertes.fr/hal-00692455
https://doi.org/10.1111/j.1365-3121.2012.01058.x
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