Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust
Quartz formation processes in the Icelandic crust were assessed using coupled δ18O and δ30Si systematics of silica deposits formed over a wide temperature range (<150 to >550 °C). Magmatic quartz reveals δ18O (-5.6 to +6.6 ‰) and δ30Si (-0.4 ± 0.2 ‰) values representative of mantle- and crusta...
Published in: | Geochemical Perspectives Letters |
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European Association of Geochemistry
2018
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Online Access: | https://hdl.handle.net/20.500.11815/855 https://doi.org/10.7185/geochemlet.1811 |
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ftopinvisindi:oai:opinvisindi.is:20.500.11815/855 2023-05-15T16:50:21+02:00 Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust Kleine, Barbara Irene Stefansson, Andri Halldórsson, Sæmundur Ari Whitehouse, M.J. Jónasson, Kristján Jarðvísindastofnun (HÍ) Institute of Earth Sciences (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland 2018-04 5-11 https://hdl.handle.net/20.500.11815/855 https://doi.org/10.7185/geochemlet.1811 en eng European Association of Geochemistry Geochemical Perspectives Letters;7 http://www.geochemicalperspectivesletters.org/article1811 Kleine, B. I., Stefánsson, A., Halldórsson, S. A., Whitehouse, M. J., & Jónasson, K. (2018). Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust. Geochemical Perspectives Letters, 7, 5-11. doi:/10.7185/geochemlet.1811 2410-339X 2410-3403 (eISSN) https://hdl.handle.net/20.500.11815/855 Geochemical Perspectives Letters doi:10.7185/geochemlet.1811 info:eu-repo/semantics/openAccess Silicon isotopes Oxygen isotopes SIMS Quartz Isotope modelling Hydrothermal fluid Kvars Kristallafræði Jarðskorpa Jarðhiti info:eu-repo/semantics/article 2018 ftopinvisindi https://doi.org/20.500.11815/855 https://doi.org/10.7185/geochemlet.1811 2022-11-18T06:51:40Z Quartz formation processes in the Icelandic crust were assessed using coupled δ18O and δ30Si systematics of silica deposits formed over a wide temperature range (<150 to >550 °C). Magmatic quartz reveals δ18O (-5.6 to +6.6 ‰) and δ30Si (-0.4 ± 0.2 ‰) values representative of mantle- and crustally-derived melts in Iceland. Hydrothermal quartz and silica polymorphs display a larger range of δ18O (-9.3 to +30.1 ‰) and δ30Si (-4.6 to +0.7 ‰) values. Isotope modelling reveals that such large variations are consistent with variable water sources and equilibrium isotope fractionation between fluids and quartz associated with secondary processes occurring in the crust, including fluid-rock interaction, boiling and cooling. In context of published δ18O and δ30Si data on hydrothermal silica deposits, we demonstrate that large ranges in δ30Si values coupled to insignificant δ18O variations may result from silica precipitation in a hydrothermal fluid conduit associated with near-surface cooling. While equilibrium isotope fractionation between fluids and quartz seems to prevail at high temperatures, kinetic fractionation likely influences isotope systematics at low temperatures. This project was financially supported by NordVulk and Landsvirkjun. Peer Reviewed Article in Journal/Newspaper Iceland Opin vísindi (Iceland) Geochemical Perspectives Letters 5 11 |
institution |
Open Polar |
collection |
Opin vísindi (Iceland) |
op_collection_id |
ftopinvisindi |
language |
English |
topic |
Silicon isotopes Oxygen isotopes SIMS Quartz Isotope modelling Hydrothermal fluid Kvars Kristallafræði Jarðskorpa Jarðhiti |
spellingShingle |
Silicon isotopes Oxygen isotopes SIMS Quartz Isotope modelling Hydrothermal fluid Kvars Kristallafræði Jarðskorpa Jarðhiti Kleine, Barbara Irene Stefansson, Andri Halldórsson, Sæmundur Ari Whitehouse, M.J. Jónasson, Kristján Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust |
topic_facet |
Silicon isotopes Oxygen isotopes SIMS Quartz Isotope modelling Hydrothermal fluid Kvars Kristallafræði Jarðskorpa Jarðhiti |
description |
Quartz formation processes in the Icelandic crust were assessed using coupled δ18O and δ30Si systematics of silica deposits formed over a wide temperature range (<150 to >550 °C). Magmatic quartz reveals δ18O (-5.6 to +6.6 ‰) and δ30Si (-0.4 ± 0.2 ‰) values representative of mantle- and crustally-derived melts in Iceland. Hydrothermal quartz and silica polymorphs display a larger range of δ18O (-9.3 to +30.1 ‰) and δ30Si (-4.6 to +0.7 ‰) values. Isotope modelling reveals that such large variations are consistent with variable water sources and equilibrium isotope fractionation between fluids and quartz associated with secondary processes occurring in the crust, including fluid-rock interaction, boiling and cooling. In context of published δ18O and δ30Si data on hydrothermal silica deposits, we demonstrate that large ranges in δ30Si values coupled to insignificant δ18O variations may result from silica precipitation in a hydrothermal fluid conduit associated with near-surface cooling. While equilibrium isotope fractionation between fluids and quartz seems to prevail at high temperatures, kinetic fractionation likely influences isotope systematics at low temperatures. This project was financially supported by NordVulk and Landsvirkjun. Peer Reviewed |
author2 |
Jarðvísindastofnun (HÍ) Institute of Earth Sciences (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland |
format |
Article in Journal/Newspaper |
author |
Kleine, Barbara Irene Stefansson, Andri Halldórsson, Sæmundur Ari Whitehouse, M.J. Jónasson, Kristján |
author_facet |
Kleine, Barbara Irene Stefansson, Andri Halldórsson, Sæmundur Ari Whitehouse, M.J. Jónasson, Kristján |
author_sort |
Kleine, Barbara Irene |
title |
Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust |
title_short |
Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust |
title_full |
Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust |
title_fullStr |
Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust |
title_full_unstemmed |
Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust |
title_sort |
silicon and oxygen isotopes unravel quartz formation processes in the icelandic crust |
publisher |
European Association of Geochemistry |
publishDate |
2018 |
url |
https://hdl.handle.net/20.500.11815/855 https://doi.org/10.7185/geochemlet.1811 |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
Geochemical Perspectives Letters;7 http://www.geochemicalperspectivesletters.org/article1811 Kleine, B. I., Stefánsson, A., Halldórsson, S. A., Whitehouse, M. J., & Jónasson, K. (2018). Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust. Geochemical Perspectives Letters, 7, 5-11. doi:/10.7185/geochemlet.1811 2410-339X 2410-3403 (eISSN) https://hdl.handle.net/20.500.11815/855 Geochemical Perspectives Letters doi:10.7185/geochemlet.1811 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/20.500.11815/855 https://doi.org/10.7185/geochemlet.1811 |
container_title |
Geochemical Perspectives Letters |
container_start_page |
5 |
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11 |
_version_ |
1766040509516611584 |