Backward tracking of gas chemistry measurements at Erebus volcano
نویسندگان
چکیده
Clive Oppenheimer ISTO, UMR 7327, CNRS/INSU, FR-45071 Orléans, France ISTO, UMR 7327, Université d’Orléans, FR-45071 Orléans, France ISTO, UMR 7327, BRGM, FR-45071 Orléans, France Institute for Advanced Studies, Le Studium, Orléans, France Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK Marina Alletti ISTO, UMR 7327, CNRS/INSU, FR-45071 Orléans, France ISTO, UMR 7327, Université d’Orléans, FR-45071 Orléans, France ISTO, UMR 7327, BRGM, FR-45071 Orléans, France Philip R. Kyle Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, New Mexico 87801, USA Bruno Scaillet ISTO, UMR 7327, CNRS/INSU, FR-45071 Orléans, France ISTO, UMR 7327, Université d’Orléans, FR-45071 Orléans, France ISTO, UMR 7327, BRGM, FR-45071 Orléans, France Michael R. Carroll Department of Earth Sciences, University of Camerino, IT-62302 Camerino, Italy
منابع مشابه
Eruptive history and magmatic stability of Erebus volcano, Antarctica: Insights from englacial tephra
A tephrostratigraphy of the active Antarctic volcano, Mt. Erebus, was determined from englacial tephra on the ice-covered flanks of Erebus and an adjacent volcano. The tephra are, used to reconstruct the eruptive history and magmatic evolution of Erebus. Scanning electron microscope images and Image Particle Analysis suggest the tephra formed in phreatomagmatic and magmatic eruptions and in som...
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