Storage and evolution of mafic and intermediate alkaline magmas beneath ross Island, Antarctica ...
We present the results of phase equilibrium experiments carried out on basanite and phonotephrite lavas from Ross Island, Antarctica. Experiments were designed to reproduce the P-T-X-fO₂ conditions of deep and intermediate magma storage and to place constraints on the differentiation of each of the...
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ftdatacite:10.17863/cam.6946 2024-02-27T08:35:11+00:00 Storage and evolution of mafic and intermediate alkaline magmas beneath ross Island, Antarctica ... Iacovino, K Oppenheimer, C Scaillet, B Kyle, P 2016 https://dx.doi.org/10.17863/cam.6946 https://www.repository.cam.ac.uk/handle/1810/261735 en eng Oxford University Press open.access Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 alkaline volcanism basanite CO₂ phase equilibria phonotephrite Ross Island article-journal ScholarlyArticle JournalArticle Article 2016 ftdatacite https://doi.org/10.17863/cam.6946 2024-02-01T14:54:53Z We present the results of phase equilibrium experiments carried out on basanite and phonotephrite lavas from Ross Island, Antarctica. Experiments were designed to reproduce the P-T-X-fO₂ conditions of deep and intermediate magma storage and to place constraints on the differentiation of each of the two predominant lava suites on the island, which are thought to be derived from a common parent melt. The Erebus Lineage (EL) consists of lava erupted from the Erebus summit and the Dry Valley Drilling Project (DVDP) lineage is represented by lavas sampled by drill core on Hut Point Peninsula. Experiments were performed in internally heated pressure vessels over a range of temperatures (1000-1150°C) and pressures (200-400 MPa), under oxidized conditions (NNO to NNO+3, where NNO is the nickel-nickel oxide buffer), with X_Η2O of the H₂O-CO₂ mixture added to the experimental capsule varying between zero and unity. The overall mineralogy and mineral compositions of the natural lavas were reproduced, suggesting ... Article in Journal/Newspaper Antarc* Antarctica Ross Island DataCite Metadata Store (German National Library of Science and Technology) Hut Point ENVELOPE(166.850,166.850,-77.767,-77.767) Hut Point Peninsula ENVELOPE(166.850,166.850,-77.767,-77.767) Ross Island |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
alkaline volcanism basanite CO₂ phase equilibria phonotephrite Ross Island |
spellingShingle |
alkaline volcanism basanite CO₂ phase equilibria phonotephrite Ross Island Iacovino, K Oppenheimer, C Scaillet, B Kyle, P Storage and evolution of mafic and intermediate alkaline magmas beneath ross Island, Antarctica ... |
topic_facet |
alkaline volcanism basanite CO₂ phase equilibria phonotephrite Ross Island |
description |
We present the results of phase equilibrium experiments carried out on basanite and phonotephrite lavas from Ross Island, Antarctica. Experiments were designed to reproduce the P-T-X-fO₂ conditions of deep and intermediate magma storage and to place constraints on the differentiation of each of the two predominant lava suites on the island, which are thought to be derived from a common parent melt. The Erebus Lineage (EL) consists of lava erupted from the Erebus summit and the Dry Valley Drilling Project (DVDP) lineage is represented by lavas sampled by drill core on Hut Point Peninsula. Experiments were performed in internally heated pressure vessels over a range of temperatures (1000-1150°C) and pressures (200-400 MPa), under oxidized conditions (NNO to NNO+3, where NNO is the nickel-nickel oxide buffer), with X_Η2O of the H₂O-CO₂ mixture added to the experimental capsule varying between zero and unity. The overall mineralogy and mineral compositions of the natural lavas were reproduced, suggesting ... |
format |
Article in Journal/Newspaper |
author |
Iacovino, K Oppenheimer, C Scaillet, B Kyle, P |
author_facet |
Iacovino, K Oppenheimer, C Scaillet, B Kyle, P |
author_sort |
Iacovino, K |
title |
Storage and evolution of mafic and intermediate alkaline magmas beneath ross Island, Antarctica ... |
title_short |
Storage and evolution of mafic and intermediate alkaline magmas beneath ross Island, Antarctica ... |
title_full |
Storage and evolution of mafic and intermediate alkaline magmas beneath ross Island, Antarctica ... |
title_fullStr |
Storage and evolution of mafic and intermediate alkaline magmas beneath ross Island, Antarctica ... |
title_full_unstemmed |
Storage and evolution of mafic and intermediate alkaline magmas beneath ross Island, Antarctica ... |
title_sort |
storage and evolution of mafic and intermediate alkaline magmas beneath ross island, antarctica ... |
publisher |
Oxford University Press |
publishDate |
2016 |
url |
https://dx.doi.org/10.17863/cam.6946 https://www.repository.cam.ac.uk/handle/1810/261735 |
long_lat |
ENVELOPE(166.850,166.850,-77.767,-77.767) ENVELOPE(166.850,166.850,-77.767,-77.767) |
geographic |
Hut Point Hut Point Peninsula Ross Island |
geographic_facet |
Hut Point Hut Point Peninsula Ross Island |
genre |
Antarc* Antarctica Ross Island |
genre_facet |
Antarc* Antarctica Ross Island |
op_rights |
open.access Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.6946 |
_version_ |
1792041651043041280 |