Mantle to surface degassing of alkalic magmas at Erebus volcano, Antarctica
International audience Continental intraplate volcanoes, such as Erebus volcano, Antarctica, are associated with extensional tectonics, mantle upwelling and high heat flow. Typically, erupted magmas are alkaline and rich in volatiles (especially CO2), inherited from low degrees of partial melting of...
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Bibliographic Details
Published in: | Earth and Planetary Science Letters |
Main Authors: |
Oppenheimer, Clive,
Moretti, Roberto,
Kyle, Philip R.,
Eschenbacher, Al,
Lowenstern, Jacob B.,
Hervig, Richard L.,
Dunbar, Nelia W. |
Other Authors: |
University of Cambridge UK (CAM),
Institut des Sciences de la Terre d'Orléans (ISTO),
Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours-Centre National de la Recherche Scientifique (CNRS),
Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Napoli (INGV),
Istituto Nazionale di Geofisica e Vulcanologia,
Centro Interdipartimentale di Ricerca in Ingegneria Ambientale (CIRIAM),
Seconda Università degli studi di Napoli,
New Mexico Institute of Mining and Technology New Mexico Tech (NMT),
Volcano Hazards Team,
United States Geological Survey Reston (USGS),
ASU School of Earth and Space Exploration (SESE),
Arizona State University Tempe (ASU),
ANT-0538414 and ANT-0838817 from the Office of Polar Programs (National Science Foundation) |
Format: | Article in Journal/Newspaper
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Language: | English |
Published: |
HAL CCSD
2011
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Subjects: |
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Online Access: | https://hal-insu.archives-ouvertes.fr/insu-00707142
https://hal-insu.archives-ouvertes.fr/insu-00707142/document
https://hal-insu.archives-ouvertes.fr/insu-00707142/file/Oppenheimer-EPSL-2011.pdf
https://doi.org/10.1016/j.epsl.2011.04.005
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