Structural development of migmatites near Skåldö, southwest Finland

The migmatites of the Skåldö area show the effects of an extensive polyphase deformational history at relatively deep crustal levels during the Svecokarelian episode. Despite the complexity of the fold patterns it is possible to establish a deformational sequence into which the many phases of igneou...

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Main Authors: A.M. Hopgood, D.R. Bowes, J. Addison
Format: Article
Language:English
Published: Geological Society of Finland 1976-12-01
Series:Bulletin of the Geological Society of Finland
Online Access:http://www.geologinenseura.fi/bulletin/Volume48/sgs_bt_048_1_2_pages_043_062.pdf
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author A.M. Hopgood
D.R. Bowes
J. Addison
author_facet A.M. Hopgood
D.R. Bowes
J. Addison
author_sort A.M. Hopgood
collection DOAJ
description The migmatites of the Skåldö area show the effects of an extensive polyphase deformational history at relatively deep crustal levels during the Svecokarelian episode. Despite the complexity of the fold patterns it is possible to establish a deformational sequence into which the many phases of igneous emplacement in the rocks can be placed. There are at least seven successive fold sets and a number of phases of both basic and acidic igneous activity as well as the effects of metamorphism which reached a peak, under amphibolite facies conditions, early in the deformational history. Taken together the various features comprise a complex framework which can be used as a basis for comparison and correlation with the products of the Svecokarelian orogenic episode in other parts of the Baltic Shield. The characteristics of these migmatites in this classic area, viz. their »mixed» aspect as described by J. J. Sederholm, is shown to result from their extensive deformational, metamorphic and igneous history in which tectonic and igneous activity played prominent roles.
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spelling doaj.art-3023894849a647db9ddac0c11440dde72022-12-22T02:50:40ZengGeological Society of FinlandBulletin of the Geological Society of Finland0367-52111799-46321976-12-01481-2436210.17741/bgsf/48.1-2.005Structural development of migmatites near Skåldö, southwest FinlandA.M. HopgoodD.R. BowesJ. AddisonThe migmatites of the Skåldö area show the effects of an extensive polyphase deformational history at relatively deep crustal levels during the Svecokarelian episode. Despite the complexity of the fold patterns it is possible to establish a deformational sequence into which the many phases of igneous emplacement in the rocks can be placed. There are at least seven successive fold sets and a number of phases of both basic and acidic igneous activity as well as the effects of metamorphism which reached a peak, under amphibolite facies conditions, early in the deformational history. Taken together the various features comprise a complex framework which can be used as a basis for comparison and correlation with the products of the Svecokarelian orogenic episode in other parts of the Baltic Shield. The characteristics of these migmatites in this classic area, viz. their »mixed» aspect as described by J. J. Sederholm, is shown to result from their extensive deformational, metamorphic and igneous history in which tectonic and igneous activity played prominent roles.http://www.geologinenseura.fi/bulletin/Volume48/sgs_bt_048_1_2_pages_043_062.pdf
spellingShingle A.M. Hopgood
D.R. Bowes
J. Addison
Structural development of migmatites near Skåldö, southwest Finland
Bulletin of the Geological Society of Finland
title Structural development of migmatites near Skåldö, southwest Finland
title_full Structural development of migmatites near Skåldö, southwest Finland
title_fullStr Structural development of migmatites near Skåldö, southwest Finland
title_full_unstemmed Structural development of migmatites near Skåldö, southwest Finland
title_short Structural development of migmatites near Skåldö, southwest Finland
title_sort structural development of migmatites near skaldo southwest finland
url http://www.geologinenseura.fi/bulletin/Volume48/sgs_bt_048_1_2_pages_043_062.pdf
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