Proterozoic crustal evolution in southcentral Fennoscandia
The Transscandinavian Igneous Belt (TIB) and the Eastern Segment of the Southwest Scandinavian Domain reflect advanced stages of continental growth within the Fennoscandian Shield. The relationship between the two units is not clear, mainly because N-S trending shear zones of the Protogine Zone tran...
Main Author: | |
---|---|
Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
Published: |
2010
|
Subjects: | |
Online Access: | http://hdl.handle.net/2077/21530 |
id |
ftunivgoeteborg:oai:gupea.ub.gu.se:2077/21530 |
---|---|
record_format |
openpolar |
spelling |
ftunivgoeteborg:oai:gupea.ub.gu.se:2077/21530 2023-10-29T02:36:16+01:00 Proterozoic crustal evolution in southcentral Fennoscandia Appelquist, Karin 2010-01-13T15:26:05Z application/msword application/pdf http://hdl.handle.net/2077/21530 eng eng A130 I: Appelquist, K., Cornell, D. & Brander, L., 2008. Age, tectonic setting and petrogenesis of the Habo Volcanic Suite: Evidence for an active continental margin setting for the Transscandinavian Igneous Belt. GFF 130, 123-138. II: Appelquist, K., Eliasson, T., Bergström, U. & Rimša, A. The Palaeoproterozoic Malmbäck Formation in S Sweden: age, composition and tectonic setting. GFF 131, 229-243. ::doi::10.1080/11035890903189777 III: Appelquist, K. & Johansson, Å. Nd isotope systematics of 1.8 Ga volcanic rocks within the Transscandinavian Igneous Belt, southcentral Sweden. Submitted to GFF. IV: Brander, L., Appelquist, K., Cornell, D. & Andersson, U.B. 1.71-1.60 Ga crust formation and 1.46-1.41 Ga Hallandian-Danopolonian deformation – a 300 Ma common history of the Transscandinavian Igneous Belt and the Eastern Segment. Manuscript. V: Appelquist, K., Brander, L., Johansson, Å., Andersson, U.B. & Cornell, D. Geochemical and Sm-Nd isotope signatures of granitoids from the Transscandinavian Igneous Belt and the Eastern Segment of Sweden. Submitted to Geological Journal. 978-91-628-7906-8 1400-3813 http://hdl.handle.net/2077/21530 Transscandinavian Igneous Belt TIB Eastern Segment Habo Volcanic Suite Malmbäck Formation U-Pb zircon ion probe dating Nd isotopes geochemistry Hallandian Danopolonian Text Doctoral thesis Doctor of Philosophy 2010 ftunivgoeteborg 2023-10-04T21:22:30Z The Transscandinavian Igneous Belt (TIB) and the Eastern Segment of the Southwest Scandinavian Domain reflect advanced stages of continental growth within the Fennoscandian Shield. The relationship between the two units is not clear, mainly because N-S trending shear zones of the Protogine Zone transect the border zone. The main goal of this thesis has been to investigate rocks in the border zone and to conclude how these rocks differ from each other. In this work two volcanic sequences and 24 granitoids in the border area, near Jönköping, were examined. The thesis reports geochemical and Sm-Nd isotope data as well as U-Pb ion microprobe zircon dates for extrusive and intrusive rocks in the southwestern part of the TIB and intrusive rocks in the eastern part of the southern Eastern Segment. The TIB rocks are subdivided into TIB-0, TIB-1 and TIB-2 groups based on their ages. In this work, the Habo Volcanic Suite and the Malmbäck Formation are dated at 1795±13 Ma and 1796±7 Ma respectively, which establishes that they are part of the TIB-1 volcanic rocks. The Malmbäck Formation is situated in the southwestern part of TIB, east of the Protogine Zone, whereas the Habo Volcanic Suite is located c. 50 km northwest of the Malmbäck Formation, between shear zones of the Protogine Zone. Both suites comprise mafic to felsic components and the Malmbäck Formation includes one of the largest mafic volcanic rock units of the TIB-1. The Malmbäck Formation comprises fairly well preserved volcanic rocks, with primary textures, although mineral parageneses in some rocks suggest metamorphism at up to epidote-amphibolite facies conditions. Amphibolites facies metamorphism and deformation has largely obscured primary textures of the Habo Volcanic Suite. Dating of a Barnarp granite which intrudes the Habo Volcanic Suite gave an age of 1660±9 Ma, corresponding to TIB-2. The occurrences of Malmbäck Formation megaxenoliths within TIB-1 granitoids are explained by stoping. Geochemical signatures of the two metavolcanic rock suites suggest ... Doctoral or Postdoctoral Thesis Fennoscandia Fennoscandian University of Gothenburg: GUPEA (Gothenburg University Publications Electronic Archive) |
institution |
Open Polar |
collection |
University of Gothenburg: GUPEA (Gothenburg University Publications Electronic Archive) |
op_collection_id |
ftunivgoeteborg |
language |
English |
topic |
Transscandinavian Igneous Belt TIB Eastern Segment Habo Volcanic Suite Malmbäck Formation U-Pb zircon ion probe dating Nd isotopes geochemistry Hallandian Danopolonian |
spellingShingle |
Transscandinavian Igneous Belt TIB Eastern Segment Habo Volcanic Suite Malmbäck Formation U-Pb zircon ion probe dating Nd isotopes geochemistry Hallandian Danopolonian Appelquist, Karin Proterozoic crustal evolution in southcentral Fennoscandia |
topic_facet |
Transscandinavian Igneous Belt TIB Eastern Segment Habo Volcanic Suite Malmbäck Formation U-Pb zircon ion probe dating Nd isotopes geochemistry Hallandian Danopolonian |
description |
The Transscandinavian Igneous Belt (TIB) and the Eastern Segment of the Southwest Scandinavian Domain reflect advanced stages of continental growth within the Fennoscandian Shield. The relationship between the two units is not clear, mainly because N-S trending shear zones of the Protogine Zone transect the border zone. The main goal of this thesis has been to investigate rocks in the border zone and to conclude how these rocks differ from each other. In this work two volcanic sequences and 24 granitoids in the border area, near Jönköping, were examined. The thesis reports geochemical and Sm-Nd isotope data as well as U-Pb ion microprobe zircon dates for extrusive and intrusive rocks in the southwestern part of the TIB and intrusive rocks in the eastern part of the southern Eastern Segment. The TIB rocks are subdivided into TIB-0, TIB-1 and TIB-2 groups based on their ages. In this work, the Habo Volcanic Suite and the Malmbäck Formation are dated at 1795±13 Ma and 1796±7 Ma respectively, which establishes that they are part of the TIB-1 volcanic rocks. The Malmbäck Formation is situated in the southwestern part of TIB, east of the Protogine Zone, whereas the Habo Volcanic Suite is located c. 50 km northwest of the Malmbäck Formation, between shear zones of the Protogine Zone. Both suites comprise mafic to felsic components and the Malmbäck Formation includes one of the largest mafic volcanic rock units of the TIB-1. The Malmbäck Formation comprises fairly well preserved volcanic rocks, with primary textures, although mineral parageneses in some rocks suggest metamorphism at up to epidote-amphibolite facies conditions. Amphibolites facies metamorphism and deformation has largely obscured primary textures of the Habo Volcanic Suite. Dating of a Barnarp granite which intrudes the Habo Volcanic Suite gave an age of 1660±9 Ma, corresponding to TIB-2. The occurrences of Malmbäck Formation megaxenoliths within TIB-1 granitoids are explained by stoping. Geochemical signatures of the two metavolcanic rock suites suggest ... |
format |
Doctoral or Postdoctoral Thesis |
author |
Appelquist, Karin |
author_facet |
Appelquist, Karin |
author_sort |
Appelquist, Karin |
title |
Proterozoic crustal evolution in southcentral Fennoscandia |
title_short |
Proterozoic crustal evolution in southcentral Fennoscandia |
title_full |
Proterozoic crustal evolution in southcentral Fennoscandia |
title_fullStr |
Proterozoic crustal evolution in southcentral Fennoscandia |
title_full_unstemmed |
Proterozoic crustal evolution in southcentral Fennoscandia |
title_sort |
proterozoic crustal evolution in southcentral fennoscandia |
publishDate |
2010 |
url |
http://hdl.handle.net/2077/21530 |
genre |
Fennoscandia Fennoscandian |
genre_facet |
Fennoscandia Fennoscandian |
op_relation |
A130 I: Appelquist, K., Cornell, D. & Brander, L., 2008. Age, tectonic setting and petrogenesis of the Habo Volcanic Suite: Evidence for an active continental margin setting for the Transscandinavian Igneous Belt. GFF 130, 123-138. II: Appelquist, K., Eliasson, T., Bergström, U. & Rimša, A. The Palaeoproterozoic Malmbäck Formation in S Sweden: age, composition and tectonic setting. GFF 131, 229-243. ::doi::10.1080/11035890903189777 III: Appelquist, K. & Johansson, Å. Nd isotope systematics of 1.8 Ga volcanic rocks within the Transscandinavian Igneous Belt, southcentral Sweden. Submitted to GFF. IV: Brander, L., Appelquist, K., Cornell, D. & Andersson, U.B. 1.71-1.60 Ga crust formation and 1.46-1.41 Ga Hallandian-Danopolonian deformation – a 300 Ma common history of the Transscandinavian Igneous Belt and the Eastern Segment. Manuscript. V: Appelquist, K., Brander, L., Johansson, Å., Andersson, U.B. & Cornell, D. Geochemical and Sm-Nd isotope signatures of granitoids from the Transscandinavian Igneous Belt and the Eastern Segment of Sweden. Submitted to Geological Journal. 978-91-628-7906-8 1400-3813 http://hdl.handle.net/2077/21530 |
_version_ |
1781059997039329280 |