Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics
In situ Lu-Hf (laser ablation microprobe-inductively coupled plasma mass spectrometry (LAMICPMS)) and U-Pb (LAM-ICPMS, secondary ionization mass spectrometry (SIMS)) analyses of zircon, and whole-rock Sm-Nd isotope analyses were performed on rocks formed during magmatic events in three Archaean comp...
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/d723defe-b019-45be-b746-fd870452133b 2024-06-02T08:06:29+00:00 Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics Lauri, Laura S. Andersen, Tom Hölttä, Pentti Huhma, Hannu Graham, Stuart 2011-01 https://researchers.mq.edu.au/en/publications/d723defe-b019-45be-b746-fd870452133b https://doi.org/10.1144/0016-76492009-159 http://www.scopus.com/inward/record.url?scp=84860389236&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Lauri , L S , Andersen , T , Hölttä , P , Huhma , H & Graham , S 2011 , ' Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics ' , Journal of the Geological Society , vol. 168 , no. 1 , pp. 201-218 . https://doi.org/10.1144/0016-76492009-159 article 2011 ftmacquarieunicr https://doi.org/10.1144/0016-76492009-159 2024-05-07T03:23:29Z In situ Lu-Hf (laser ablation microprobe-inductively coupled plasma mass spectrometry (LAMICPMS)) and U-Pb (LAM-ICPMS, secondary ionization mass spectrometry (SIMS)) analyses of zircon, and whole-rock Sm-Nd isotope analyses were performed on rocks formed during magmatic events in three Archaean complexes in the Karelian Province of Fennoscandia (Pudasjärvi, Koillismaa and Iisalmi). These complexes have U-Pb ages ranging from 3.5 to 2.6 Ga. In Pudasjärvi, sparse xenocrystic cores give ages of 3.6-3.7 Ga and initial 176 Hf/ 177 Hf suggesting influence of a crustal component T ≥ 4.0 Ga (assuming a CHUR-like mantle source). Ages and Nd and Hf isotope patterns indicate magmatic events at 3.6-3.7 Ga (Siurua, Pudasjärvi with ≥4.0 Ga precursor), 3.2 Ga (Iisalmi, Koillismaa), 2.8 Ga (Pudasjärvi) and 2.7 Ga (Pudasjärvi, Iisalmi). In the Meso- and Palaeoarchaean events, there is no evidence of sources equivalent to present-day depleted mantle; such sources were, however, involved in the 2.8-2.7 Ga events. Hf and Nd are strongly correlated. Contrasts between the Archaean complexes indicate that they evolved separately until c. 2.7 Ga. The age and Hf pattern of ≤2.8 Ga rocks in the Karelian Province is compatible with a scenario in which the Karelia, Superior, Yilgarn and Slave cratons were part of a late Archaean supercontinent, but does not constitute proof of the existence of such a supercontinent. Article in Journal/Newspaper Fennoscandia Fennoscandian karelian Macquarie University Research Portal Koillismaa ENVELOPE(29.047,29.047,65.843,65.843) Journal of the Geological Society 168 1 201 218 |
institution |
Open Polar |
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Macquarie University Research Portal |
op_collection_id |
ftmacquarieunicr |
language |
English |
description |
In situ Lu-Hf (laser ablation microprobe-inductively coupled plasma mass spectrometry (LAMICPMS)) and U-Pb (LAM-ICPMS, secondary ionization mass spectrometry (SIMS)) analyses of zircon, and whole-rock Sm-Nd isotope analyses were performed on rocks formed during magmatic events in three Archaean complexes in the Karelian Province of Fennoscandia (Pudasjärvi, Koillismaa and Iisalmi). These complexes have U-Pb ages ranging from 3.5 to 2.6 Ga. In Pudasjärvi, sparse xenocrystic cores give ages of 3.6-3.7 Ga and initial 176 Hf/ 177 Hf suggesting influence of a crustal component T ≥ 4.0 Ga (assuming a CHUR-like mantle source). Ages and Nd and Hf isotope patterns indicate magmatic events at 3.6-3.7 Ga (Siurua, Pudasjärvi with ≥4.0 Ga precursor), 3.2 Ga (Iisalmi, Koillismaa), 2.8 Ga (Pudasjärvi) and 2.7 Ga (Pudasjärvi, Iisalmi). In the Meso- and Palaeoarchaean events, there is no evidence of sources equivalent to present-day depleted mantle; such sources were, however, involved in the 2.8-2.7 Ga events. Hf and Nd are strongly correlated. Contrasts between the Archaean complexes indicate that they evolved separately until c. 2.7 Ga. The age and Hf pattern of ≤2.8 Ga rocks in the Karelian Province is compatible with a scenario in which the Karelia, Superior, Yilgarn and Slave cratons were part of a late Archaean supercontinent, but does not constitute proof of the existence of such a supercontinent. |
format |
Article in Journal/Newspaper |
author |
Lauri, Laura S. Andersen, Tom Hölttä, Pentti Huhma, Hannu Graham, Stuart |
spellingShingle |
Lauri, Laura S. Andersen, Tom Hölttä, Pentti Huhma, Hannu Graham, Stuart Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics |
author_facet |
Lauri, Laura S. Andersen, Tom Hölttä, Pentti Huhma, Hannu Graham, Stuart |
author_sort |
Lauri, Laura S. |
title |
Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics |
title_short |
Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics |
title_full |
Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics |
title_fullStr |
Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics |
title_full_unstemmed |
Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics |
title_sort |
evolution of the archaean karelian province in the fennoscandian shield in the light of u-pb zircon ages and sm-nd and lu-hf isotope systematics |
publishDate |
2011 |
url |
https://researchers.mq.edu.au/en/publications/d723defe-b019-45be-b746-fd870452133b https://doi.org/10.1144/0016-76492009-159 http://www.scopus.com/inward/record.url?scp=84860389236&partnerID=8YFLogxK |
long_lat |
ENVELOPE(29.047,29.047,65.843,65.843) |
geographic |
Koillismaa |
geographic_facet |
Koillismaa |
genre |
Fennoscandia Fennoscandian karelian |
genre_facet |
Fennoscandia Fennoscandian karelian |
op_source |
Lauri , L S , Andersen , T , Hölttä , P , Huhma , H & Graham , S 2011 , ' Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics ' , Journal of the Geological Society , vol. 168 , no. 1 , pp. 201-218 . https://doi.org/10.1144/0016-76492009-159 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1144/0016-76492009-159 |
container_title |
Journal of the Geological Society |
container_volume |
168 |
container_issue |
1 |
container_start_page |
201 |
op_container_end_page |
218 |
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1800751437560414208 |