Continental crust beneath southeast Iceland
The Iceland hotspot is widely thought to be the surface expression of a deep mantle plume from the core–mantle boundary that can be traced back in time at least 62 My. However, some lavas contain continental material, which has previously been proposed to have been recycled through the plume. Here,...
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Online Access: | http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4403175/ http://www.ncbi.nlm.nih.gov/pubmed/25825769 https://doi.org/10.1073/pnas.1423099112 |
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ftpubmed:oai:pubmedcentral.nih.gov:4403175 2023-05-15T16:27:56+02:00 Continental crust beneath southeast Iceland Torsvik, Trond H. Amundsen, Hans E. F. Trønnes, Reidar G. Doubrovine, Pavel V. Gaina, Carmen Kusznir, Nick J. Steinberger, Bernhard Corfu, Fernando Ashwal, Lewis D. Griffin, William L. Werner, Stephanie C. Jamtveit, Bjørn 2015-04-14 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4403175/ http://www.ncbi.nlm.nih.gov/pubmed/25825769 https://doi.org/10.1073/pnas.1423099112 en eng National Academy of Sciences http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4403175/ http://www.ncbi.nlm.nih.gov/pubmed/25825769 http://dx.doi.org/10.1073/pnas.1423099112 Freely available online through the PNAS open access option. PNAS Plus Text 2015 ftpubmed https://doi.org/10.1073/pnas.1423099112 2015-04-26T00:08:51Z The Iceland hotspot is widely thought to be the surface expression of a deep mantle plume from the core–mantle boundary that can be traced back in time at least 62 My. However, some lavas contain continental material, which has previously been proposed to have been recycled through the plume. Here, we argue that the plume split off a sliver of continent from Greenland in the Early Eocene. This sliver is now located beneath southeast Iceland where it locally contaminates some of the plume-derived magmas. Text Greenland Iceland PubMed Central (PMC) Greenland Proceedings of the National Academy of Sciences 112 15 E1818 E1827 |
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PubMed Central (PMC) |
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PNAS Plus Torsvik, Trond H. Amundsen, Hans E. F. Trønnes, Reidar G. Doubrovine, Pavel V. Gaina, Carmen Kusznir, Nick J. Steinberger, Bernhard Corfu, Fernando Ashwal, Lewis D. Griffin, William L. Werner, Stephanie C. Jamtveit, Bjørn Continental crust beneath southeast Iceland |
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PNAS Plus |
description |
The Iceland hotspot is widely thought to be the surface expression of a deep mantle plume from the core–mantle boundary that can be traced back in time at least 62 My. However, some lavas contain continental material, which has previously been proposed to have been recycled through the plume. Here, we argue that the plume split off a sliver of continent from Greenland in the Early Eocene. This sliver is now located beneath southeast Iceland where it locally contaminates some of the plume-derived magmas. |
format |
Text |
author |
Torsvik, Trond H. Amundsen, Hans E. F. Trønnes, Reidar G. Doubrovine, Pavel V. Gaina, Carmen Kusznir, Nick J. Steinberger, Bernhard Corfu, Fernando Ashwal, Lewis D. Griffin, William L. Werner, Stephanie C. Jamtveit, Bjørn |
author_facet |
Torsvik, Trond H. Amundsen, Hans E. F. Trønnes, Reidar G. Doubrovine, Pavel V. Gaina, Carmen Kusznir, Nick J. Steinberger, Bernhard Corfu, Fernando Ashwal, Lewis D. Griffin, William L. Werner, Stephanie C. Jamtveit, Bjørn |
author_sort |
Torsvik, Trond H. |
title |
Continental crust beneath southeast Iceland |
title_short |
Continental crust beneath southeast Iceland |
title_full |
Continental crust beneath southeast Iceland |
title_fullStr |
Continental crust beneath southeast Iceland |
title_full_unstemmed |
Continental crust beneath southeast Iceland |
title_sort |
continental crust beneath southeast iceland |
publisher |
National Academy of Sciences |
publishDate |
2015 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4403175/ http://www.ncbi.nlm.nih.gov/pubmed/25825769 https://doi.org/10.1073/pnas.1423099112 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Iceland |
genre_facet |
Greenland Iceland |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4403175/ http://www.ncbi.nlm.nih.gov/pubmed/25825769 http://dx.doi.org/10.1073/pnas.1423099112 |
op_rights |
Freely available online through the PNAS open access option. |
op_doi |
https://doi.org/10.1073/pnas.1423099112 |
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Proceedings of the National Academy of Sciences |
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112 |
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15 |
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E1818 |
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E1827 |
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1766017525640855552 |