Multistage hydration during oceanic serpentinisation revealed by in situ oxygen isotope and trace element analyses ...
Serpentinisation of mantle peridotites below the seafloor is the most important hydration reaction in the Earth’s deep water cycle. This critical step in water–rock interaction occurs over multiple serpentinisation stages and at variable temperatures and fluid compositions. We present the first stud...
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ftdatacite:10.48350/189572 2024-03-31T07:54:03+00:00 Multistage hydration during oceanic serpentinisation revealed by in situ oxygen isotope and trace element analyses ... Vesin, Coralie Rubatto, Daniela Pettke, Thomas Deloule, Etienne 2023 https://dx.doi.org/10.48350/189572 https://boris.unibe.ch/189572/ unknown Elsevier Science https://dx.doi.org/10.1016/j.gca.2023.06.032 open access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 550 Earth sciences & geology Text journal article article-journal ScholarlyArticle 2023 ftdatacite https://doi.org/10.48350/18957210.1016/j.gca.2023.06.032 2024-03-04T12:08:03Z Serpentinisation of mantle peridotites below the seafloor is the most important hydration reaction in the Earth’s deep water cycle. This critical step in water–rock interaction occurs over multiple serpentinisation stages and at variable temperatures and fluid compositions. We present the first study using spatially coupled in-situ analysis of oxygen isotopes (secondary ionization mass spectrometry) and trace elements (laser ablation inductively coupled plasma mass spectrometry) to unravel the multistage hydration history of oceanic serpentinites. We study samples from the Newfoundland-Iberia extended passive margins, which represents a magma-poor ocean continent transition zone (Ocean Drilling Program cores, Leg 173 Site 1070 from Iberia, Leg 210 Site 1277 from Newfoundland). The concentrations of the fluid mobile elements chlorine and boron in serpentine are used as a proxy for the salinity of the serpentinising fluid. The correlation of Cl/B with δ18Oserpentine compositions provides new insights to ... Text Newfoundland DataCite Metadata Store (German National Library of Science and Technology) |
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550 Earth sciences & geology |
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550 Earth sciences & geology Vesin, Coralie Rubatto, Daniela Pettke, Thomas Deloule, Etienne Multistage hydration during oceanic serpentinisation revealed by in situ oxygen isotope and trace element analyses ... |
topic_facet |
550 Earth sciences & geology |
description |
Serpentinisation of mantle peridotites below the seafloor is the most important hydration reaction in the Earth’s deep water cycle. This critical step in water–rock interaction occurs over multiple serpentinisation stages and at variable temperatures and fluid compositions. We present the first study using spatially coupled in-situ analysis of oxygen isotopes (secondary ionization mass spectrometry) and trace elements (laser ablation inductively coupled plasma mass spectrometry) to unravel the multistage hydration history of oceanic serpentinites. We study samples from the Newfoundland-Iberia extended passive margins, which represents a magma-poor ocean continent transition zone (Ocean Drilling Program cores, Leg 173 Site 1070 from Iberia, Leg 210 Site 1277 from Newfoundland). The concentrations of the fluid mobile elements chlorine and boron in serpentine are used as a proxy for the salinity of the serpentinising fluid. The correlation of Cl/B with δ18Oserpentine compositions provides new insights to ... |
format |
Text |
author |
Vesin, Coralie Rubatto, Daniela Pettke, Thomas Deloule, Etienne |
author_facet |
Vesin, Coralie Rubatto, Daniela Pettke, Thomas Deloule, Etienne |
author_sort |
Vesin, Coralie |
title |
Multistage hydration during oceanic serpentinisation revealed by in situ oxygen isotope and trace element analyses ... |
title_short |
Multistage hydration during oceanic serpentinisation revealed by in situ oxygen isotope and trace element analyses ... |
title_full |
Multistage hydration during oceanic serpentinisation revealed by in situ oxygen isotope and trace element analyses ... |
title_fullStr |
Multistage hydration during oceanic serpentinisation revealed by in situ oxygen isotope and trace element analyses ... |
title_full_unstemmed |
Multistage hydration during oceanic serpentinisation revealed by in situ oxygen isotope and trace element analyses ... |
title_sort |
multistage hydration during oceanic serpentinisation revealed by in situ oxygen isotope and trace element analyses ... |
publisher |
Elsevier Science |
publishDate |
2023 |
url |
https://dx.doi.org/10.48350/189572 https://boris.unibe.ch/189572/ |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
https://dx.doi.org/10.1016/j.gca.2023.06.032 |
op_rights |
open access Creative Commons Attribution 4.0 International 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/10.48350/18957210.1016/j.gca.2023.06.032 |
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1795034617498042368 |