Structural evolution of the Vuotso area, Finnish Lapland

The Vuotso area is structurally interesting because the fold interference pattern in rocks of central Lapland changes into thrust-related foliation of the Lapland Granulite Belt. A felsic volcanic rock yielded a 2.45 Ga age and conformed that the volcanic rocks in the Vuotso area are (mainly) Paleop...

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Main Authors: M. Nironen, I. Mänttäri
Format: Article
Language:English
Published: Geological Society of Finland 2003-12-01
Series:Bulletin of the Geological Society of Finland
Subjects:
Online Access:http://www.geologinenseura.fi/bulletin/Volume75/NironenManttari.pdf
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author M. Nironen
I. Mänttäri
author_facet M. Nironen
I. Mänttäri
author_sort M. Nironen
collection DOAJ
description The Vuotso area is structurally interesting because the fold interference pattern in rocks of central Lapland changes into thrust-related foliation of the Lapland Granulite Belt. A felsic volcanic rock yielded a 2.45 Ga age and conformed that the volcanic rocks in the Vuotso area are (mainly) Paleoproterozoic. A structural sequence with recumbent F2 folding and predominant S2 foliation, and an interference pattern of F3 and F4 foldings could be discerned in the supracrustal rocks. A large D3 antiform is overprinted by mafic-intermediate gneisses that form the basal part of the thrust sequence. The curving of late D3 shear zones suggests that D3 deformation may be associated with thrusting from east-northeast, but thrusting of the granulites and adjacent mafic-intermediate gneisses to their present position is interpreted as a post-D3 event.
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spelling doaj.art-ce08327090cc47e0998560a8ba8c277e2022-12-22T00:24:56ZengGeological Society of FinlandBulletin of the Geological Society of Finland0367-52111799-46322003-12-01751-29310110.17741/bgsf/75.1-2.006Structural evolution of the Vuotso area, Finnish LaplandM. NironenI. MänttäriThe Vuotso area is structurally interesting because the fold interference pattern in rocks of central Lapland changes into thrust-related foliation of the Lapland Granulite Belt. A felsic volcanic rock yielded a 2.45 Ga age and conformed that the volcanic rocks in the Vuotso area are (mainly) Paleoproterozoic. A structural sequence with recumbent F2 folding and predominant S2 foliation, and an interference pattern of F3 and F4 foldings could be discerned in the supracrustal rocks. A large D3 antiform is overprinted by mafic-intermediate gneisses that form the basal part of the thrust sequence. The curving of late D3 shear zones suggests that D3 deformation may be associated with thrusting from east-northeast, but thrusting of the granulites and adjacent mafic-intermediate gneisses to their present position is interpreted as a post-D3 event.http://www.geologinenseura.fi/bulletin/Volume75/NironenManttari.pdfstructural geologystructural analysisgranulitesgneissesmetavolcanic rocksabsolute ageU/PbPaleoproterozoicVuotsoLapland ProvinceFinland
spellingShingle M. Nironen
I. Mänttäri
Structural evolution of the Vuotso area, Finnish Lapland
Bulletin of the Geological Society of Finland
structural geology
structural analysis
granulites
gneisses
metavolcanic rocks
absolute age
U/Pb
Paleoproterozoic
Vuotso
Lapland Province
Finland
title Structural evolution of the Vuotso area, Finnish Lapland
title_full Structural evolution of the Vuotso area, Finnish Lapland
title_fullStr Structural evolution of the Vuotso area, Finnish Lapland
title_full_unstemmed Structural evolution of the Vuotso area, Finnish Lapland
title_short Structural evolution of the Vuotso area, Finnish Lapland
title_sort structural evolution of the vuotso area finnish lapland
topic structural geology
structural analysis
granulites
gneisses
metavolcanic rocks
absolute age
U/Pb
Paleoproterozoic
Vuotso
Lapland Province
Finland
url http://www.geologinenseura.fi/bulletin/Volume75/NironenManttari.pdf
work_keys_str_mv AT mnironen structuralevolutionofthevuotsoareafinnishlapland
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