Eoarchaean crustal evolution of the North Atlantic craton
Recent studies suggest extraction of juvenile crust from the mantle has been globally continuous throughout Earth’s history, but the crustal record is biased by preservation, particularly from supercontinents [e.g. 1, 2]. As a result, crust older than the first supercontinent at c. 2.7 Ga is now rar...
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ftunivportsmpubl:oai:researchportal.port.ac.uk:publications/3dbae5a5-f2d2-489c-8f33-e25637d182cb 2023-05-15T17:29:42+02:00 Eoarchaean crustal evolution of the North Atlantic craton Lancaster, Penelope J. Storey, Craig D. Hawkesworth, Chris J. 2011 application/msword https://researchportal.port.ac.uk/portal/en/publications/eoarchaean-crustal-evolution-of-the-north-atlantic-craton(3dbae5a5-f2d2-489c-8f33-e25637d182cb).html https://researchportal.port.ac.uk/ws/files/1429736/Lancaster_2011.doc http://minmag.geoscienceworld.org/content/75/3/1261.full.pdf+html eng eng info:eu-repo/semantics/openAccess Lancaster , P J , Storey , C D & Hawkesworth , C J 2011 , ' Eoarchaean crustal evolution of the North Atlantic craton ' Mineralogical Magazine , vol 75 , no. 3 , pp. 1268 . /dk/atira/pure/core/subjects/earthsci Earth Sciences article 2011 ftunivportsmpubl 2017-09-28T19:33:17Z Recent studies suggest extraction of juvenile crust from the mantle has been globally continuous throughout Earth’s history, but the crustal record is biased by preservation, particularly from supercontinents [e.g. 1, 2]. As a result, crust older than the first supercontinent at c. 2.7 Ga is now rare and frequently strongly reworked. However, younger sedimentary rocks may preserve fragments of Archaean basement by sampling wide areas, including those which have since been buried or destroyed, thereby providing a more complete record of the ancient crust. Of these sedimentary rocks, coarse basal units are most likely to preserve local basement, constraining the likely geographical distribution of those source areas and providing greater context for any detrital material. Detrital zircons have been analyzed from basal units of the Meso/Neoproterozoic to Cambrian Stoer, Sleat, Ardvreck and Morar groups in NW Scotland to evaluate basement source ages and isotopic signatures. Widespread crustal extraction is recorded in Hf model ages between 4160–1410 Ma, peaking at c. 3350 Ma, with significant crystallisation and/or reworking between 3670–1070 Ma, peaking at c. 2700 Ma. Similar crystallisation and model ages have been identified around the North Atlantic Craton, suggesting a shared, but not consanguineous, origin. All four units contain Hf model ages that imply partial reworking of Eoarchaean crust, and model ages as old as 4200 Ma from the basal Ardvreck Gp. indicate the existence of much older crust in Scotland and the greater North Atlantic Craton. Such consistency around the craton reinforces the conclusion that crustal extraction and crystallisation are continuous, large-scale processes, and have been since the very earliest Earth. Article in Journal/Newspaper North Atlantic University of Portsmouth: Portsmouth Research Portal |
institution |
Open Polar |
collection |
University of Portsmouth: Portsmouth Research Portal |
op_collection_id |
ftunivportsmpubl |
language |
English |
topic |
/dk/atira/pure/core/subjects/earthsci Earth Sciences |
spellingShingle |
/dk/atira/pure/core/subjects/earthsci Earth Sciences Lancaster, Penelope J. Storey, Craig D. Hawkesworth, Chris J. Eoarchaean crustal evolution of the North Atlantic craton |
topic_facet |
/dk/atira/pure/core/subjects/earthsci Earth Sciences |
description |
Recent studies suggest extraction of juvenile crust from the mantle has been globally continuous throughout Earth’s history, but the crustal record is biased by preservation, particularly from supercontinents [e.g. 1, 2]. As a result, crust older than the first supercontinent at c. 2.7 Ga is now rare and frequently strongly reworked. However, younger sedimentary rocks may preserve fragments of Archaean basement by sampling wide areas, including those which have since been buried or destroyed, thereby providing a more complete record of the ancient crust. Of these sedimentary rocks, coarse basal units are most likely to preserve local basement, constraining the likely geographical distribution of those source areas and providing greater context for any detrital material. Detrital zircons have been analyzed from basal units of the Meso/Neoproterozoic to Cambrian Stoer, Sleat, Ardvreck and Morar groups in NW Scotland to evaluate basement source ages and isotopic signatures. Widespread crustal extraction is recorded in Hf model ages between 4160–1410 Ma, peaking at c. 3350 Ma, with significant crystallisation and/or reworking between 3670–1070 Ma, peaking at c. 2700 Ma. Similar crystallisation and model ages have been identified around the North Atlantic Craton, suggesting a shared, but not consanguineous, origin. All four units contain Hf model ages that imply partial reworking of Eoarchaean crust, and model ages as old as 4200 Ma from the basal Ardvreck Gp. indicate the existence of much older crust in Scotland and the greater North Atlantic Craton. Such consistency around the craton reinforces the conclusion that crustal extraction and crystallisation are continuous, large-scale processes, and have been since the very earliest Earth. |
format |
Article in Journal/Newspaper |
author |
Lancaster, Penelope J. Storey, Craig D. Hawkesworth, Chris J. |
author_facet |
Lancaster, Penelope J. Storey, Craig D. Hawkesworth, Chris J. |
author_sort |
Lancaster, Penelope J. |
title |
Eoarchaean crustal evolution of the North Atlantic craton |
title_short |
Eoarchaean crustal evolution of the North Atlantic craton |
title_full |
Eoarchaean crustal evolution of the North Atlantic craton |
title_fullStr |
Eoarchaean crustal evolution of the North Atlantic craton |
title_full_unstemmed |
Eoarchaean crustal evolution of the North Atlantic craton |
title_sort |
eoarchaean crustal evolution of the north atlantic craton |
publishDate |
2011 |
url |
https://researchportal.port.ac.uk/portal/en/publications/eoarchaean-crustal-evolution-of-the-north-atlantic-craton(3dbae5a5-f2d2-489c-8f33-e25637d182cb).html https://researchportal.port.ac.uk/ws/files/1429736/Lancaster_2011.doc http://minmag.geoscienceworld.org/content/75/3/1261.full.pdf+html |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Lancaster , P J , Storey , C D & Hawkesworth , C J 2011 , ' Eoarchaean crustal evolution of the North Atlantic craton ' Mineralogical Magazine , vol 75 , no. 3 , pp. 1268 . |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1766124486067748864 |