Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland
EJH acknowledges funding from a NERC PhD studentship and the work was completed at the University of St Andrews, UK. The peralkaline to agpaitic Ilímaussaq Complex, S. Greenland, displays spectacular macrorhythmic (> 5 m) layering via the kakortokite (agpaitic nepheline syenite), which outcrops a...
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ftstandrewserep:oai:research-repository.st-andrews.ac.uk:10023/9817 2023-07-02T03:32:25+02:00 Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland Hunt, Emma J. Finch, Adrian A. Donaldson, Colin H. University of St Andrews. Earth and Environmental Sciences University of St Andrews. School of Earth & Environmental Sciences University of St Andrews. Scottish Oceans Institute University of St Andrews. St Andrews Isotope Geochemistry University of St Andrews. Marine Alliance for Science & Technology Scotland 2016-11-14T11:30:16Z 15 application/pdf http://hdl.handle.net/10023/9817 https://doi.org/10.1016/j.lithos.2016.10.023 eng eng Lithos Hunt , E J , Finch , A A & Donaldson , C H 2017 , ' Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland ' , Lithos , vol. 268-271 , pp. 1-15 . https://doi.org/10.1016/j.lithos.2016.10.023 0024-4937 PURE: 247263599 PURE UUID: f59e3d75-2fe8-4928-b800-26bd924c28e3 RIS: urn:EBF8D2270912682BDEFB38FA610C5E39 Scopus: 84996573009 ORCID: /0000-0002-3689-1517/work/38002300 WOS: 000392680400001 http://hdl.handle.net/10023/9817 https://doi.org/10.1016/j.lithos.2016.10.023 © 2016 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/). Ilímaussaq Complex Kakortokite Agpaitic Macrorhythmic layering Crystal size distribution Eudialyte-group minerals GE Environmental Sciences DAS BDC GE Journal article 2016 ftstandrewserep https://doi.org/10.1016/j.lithos.2016.10.023 2023-06-13T18:27:34Z EJH acknowledges funding from a NERC PhD studentship and the work was completed at the University of St Andrews, UK. The peralkaline to agpaitic Ilímaussaq Complex, S. Greenland, displays spectacular macrorhythmic (> 5 m) layering via the kakortokite (agpaitic nepheline syenite), which outcrops as the lowest exposed rocks in the complex. This study applies crystal size distribution (CSD) analyses and eudialyte-group mineral chemical compositions to study the marker horizon, Unit 0, and the contact to the underlying Unit − 1. Unit 0 is the best-developed unit in the kakortokites and as such is ideal for gaining insight into processes of crystal formation and growth within the layered kakortokite. The findings are consistent with a model whereby the bulk of the black and red layers developed through in situ crystallisation at the crystal mush–magma interface, whereas the white layer developed through a range of processes operating throughout the magma chamber, including density segregation (gravitational settling and flotation). Primary textures were modified through late-stage textural coarsening via grain overgrowth. An open-system model is proposed, where varying concentrations of halogens, in combination with undercooling, controlled crystal nucleation and growth to form Unit 0. Our observations suggest that the model is applicable more widely to the layering throughout the kakortokite series and potentially other layered peralkaline/agpaitic rocks around the world. Publisher PDF Peer reviewed Article in Journal/Newspaper Greenland University of St Andrews: Digital Research Repository Greenland Lithos 268-271 1 15 |
institution |
Open Polar |
collection |
University of St Andrews: Digital Research Repository |
op_collection_id |
ftstandrewserep |
language |
English |
topic |
Ilímaussaq Complex Kakortokite Agpaitic Macrorhythmic layering Crystal size distribution Eudialyte-group minerals GE Environmental Sciences DAS BDC GE |
spellingShingle |
Ilímaussaq Complex Kakortokite Agpaitic Macrorhythmic layering Crystal size distribution Eudialyte-group minerals GE Environmental Sciences DAS BDC GE Hunt, Emma J. Finch, Adrian A. Donaldson, Colin H. Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland |
topic_facet |
Ilímaussaq Complex Kakortokite Agpaitic Macrorhythmic layering Crystal size distribution Eudialyte-group minerals GE Environmental Sciences DAS BDC GE |
description |
EJH acknowledges funding from a NERC PhD studentship and the work was completed at the University of St Andrews, UK. The peralkaline to agpaitic Ilímaussaq Complex, S. Greenland, displays spectacular macrorhythmic (> 5 m) layering via the kakortokite (agpaitic nepheline syenite), which outcrops as the lowest exposed rocks in the complex. This study applies crystal size distribution (CSD) analyses and eudialyte-group mineral chemical compositions to study the marker horizon, Unit 0, and the contact to the underlying Unit − 1. Unit 0 is the best-developed unit in the kakortokites and as such is ideal for gaining insight into processes of crystal formation and growth within the layered kakortokite. The findings are consistent with a model whereby the bulk of the black and red layers developed through in situ crystallisation at the crystal mush–magma interface, whereas the white layer developed through a range of processes operating throughout the magma chamber, including density segregation (gravitational settling and flotation). Primary textures were modified through late-stage textural coarsening via grain overgrowth. An open-system model is proposed, where varying concentrations of halogens, in combination with undercooling, controlled crystal nucleation and growth to form Unit 0. Our observations suggest that the model is applicable more widely to the layering throughout the kakortokite series and potentially other layered peralkaline/agpaitic rocks around the world. Publisher PDF Peer reviewed |
author2 |
University of St Andrews. Earth and Environmental Sciences University of St Andrews. School of Earth & Environmental Sciences University of St Andrews. Scottish Oceans Institute University of St Andrews. St Andrews Isotope Geochemistry University of St Andrews. Marine Alliance for Science & Technology Scotland |
format |
Article in Journal/Newspaper |
author |
Hunt, Emma J. Finch, Adrian A. Donaldson, Colin H. |
author_facet |
Hunt, Emma J. Finch, Adrian A. Donaldson, Colin H. |
author_sort |
Hunt, Emma J. |
title |
Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland |
title_short |
Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland |
title_full |
Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland |
title_fullStr |
Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland |
title_full_unstemmed |
Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland |
title_sort |
layering in peralkaline magmas, ilímaussaq complex, s greenland |
publishDate |
2016 |
url |
http://hdl.handle.net/10023/9817 https://doi.org/10.1016/j.lithos.2016.10.023 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland |
genre_facet |
Greenland |
op_relation |
Lithos Hunt , E J , Finch , A A & Donaldson , C H 2017 , ' Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland ' , Lithos , vol. 268-271 , pp. 1-15 . https://doi.org/10.1016/j.lithos.2016.10.023 0024-4937 PURE: 247263599 PURE UUID: f59e3d75-2fe8-4928-b800-26bd924c28e3 RIS: urn:EBF8D2270912682BDEFB38FA610C5E39 Scopus: 84996573009 ORCID: /0000-0002-3689-1517/work/38002300 WOS: 000392680400001 http://hdl.handle.net/10023/9817 https://doi.org/10.1016/j.lithos.2016.10.023 |
op_rights |
© 2016 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/). |
op_doi |
https://doi.org/10.1016/j.lithos.2016.10.023 |
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Lithos |
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268-271 |
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1 |
op_container_end_page |
15 |
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1770272000370016256 |