1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment

A convergent continental margin setting with transpressional shearing was active during TIB formation in the west. Whether this shearing was instrumental in the formation of the 1.8 Ga magmatism further continentwards, or if the magmatisin in the central and eastern areas was the result of extension...

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Published in:Lithos
Main Authors: Andersson, UB, Eklund, Olav, Fröjdö, Sören, Konopelko, D
Format: Article in Journal/Newspaper
Language:unknown
Published: 2006
Subjects:
1.8 Ga mafic magmatism
carbonate metasomatism
mantle enrichment
Nd-Sr isotopes
Fennoscandian Shield
Fennoscandian
Online Access:https://research.abo.fi/en/publications/679bd064-deb3-4a97-b394-dd1c207bfdf3
https://doi.org/10.1016/j.lithos.2005.04.001
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spelling ftaboakademicris:oai:pure.atira.dk:publications/679bd064-deb3-4a97-b394-dd1c207bfdf3 2023-05-15T16:12:48+02:00 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment Andersson, UB Eklund, Olav Fröjdö, Sören Konopelko, D 2006 https://research.abo.fi/en/publications/679bd064-deb3-4a97-b394-dd1c207bfdf3 https://doi.org/10.1016/j.lithos.2005.04.001 und unknown info:eu-repo/semantics/restrictedAccess Andersson , UB , Eklund , O , Fröjdö , S & Konopelko , D 2006 , ' 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment ' , Lithos , vol. 86 , no. 1-2 , pp. 110–136 . https://doi.org/10.1016/j.lithos.2005.04.001 1.8 Ga mafic magmatism carbonate metasomatism mantle enrichment Nd-Sr isotopes Fennoscandian Shield article 2006 ftaboakademicris https://doi.org/10.1016/j.lithos.2005.04.001 2022-12-04T14:20:38Z A convergent continental margin setting with transpressional shearing was active during TIB formation in the west. Whether this shearing was instrumental in the formation of the 1.8 Ga magmatism further continentwards, or if the magmatisin in the central and eastern areas was the result of extensional collapse or plume activity is presently not known. (c) 2005 Elsevier B.V. All rights reserved. Article in Journal/Newspaper Fennoscandian Åbo Akademi University Research Portal Lithos 86 1-2 110 136
institution Open Polar
collection Åbo Akademi University Research Portal
op_collection_id ftaboakademicris
language unknown
topic 1.8 Ga mafic magmatism
carbonate metasomatism
mantle enrichment
Nd-Sr isotopes
Fennoscandian Shield
spellingShingle 1.8 Ga mafic magmatism
carbonate metasomatism
mantle enrichment
Nd-Sr isotopes
Fennoscandian Shield
Andersson, UB
Eklund, Olav
Fröjdö, Sören
Konopelko, D
1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment
topic_facet 1.8 Ga mafic magmatism
carbonate metasomatism
mantle enrichment
Nd-Sr isotopes
Fennoscandian Shield
description A convergent continental margin setting with transpressional shearing was active during TIB formation in the west. Whether this shearing was instrumental in the formation of the 1.8 Ga magmatism further continentwards, or if the magmatisin in the central and eastern areas was the result of extensional collapse or plume activity is presently not known. (c) 2005 Elsevier B.V. All rights reserved.
format Article in Journal/Newspaper
author Andersson, UB
Eklund, Olav
Fröjdö, Sören
Konopelko, D
author_facet Andersson, UB
Eklund, Olav
Fröjdö, Sören
Konopelko, D
author_sort Andersson, UB
title 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment
title_short 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment
title_full 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment
title_fullStr 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment
title_full_unstemmed 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment
title_sort 1.8 ga magmatism in the fennoscandian shield; lateral variations in subcontinental mantle enrichment
publishDate 2006
url https://research.abo.fi/en/publications/679bd064-deb3-4a97-b394-dd1c207bfdf3
https://doi.org/10.1016/j.lithos.2005.04.001
genre Fennoscandian
genre_facet Fennoscandian
op_source Andersson , UB , Eklund , O , Fröjdö , S & Konopelko , D 2006 , ' 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment ' , Lithos , vol. 86 , no. 1-2 , pp. 110–136 . https://doi.org/10.1016/j.lithos.2005.04.001
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1016/j.lithos.2005.04.001
container_title Lithos
container_volume 86
container_issue 1-2
container_start_page 110
op_container_end_page 136
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