Scotland–Finland Precambrian correlations

Isotopic age determinations indicate the generally co-eval nature of major episodes of earth history shown by the Precambrian rocks of Scotland and Finland, viz. (1) the c. 2 800—2 600 m.y. Scourian and Presvecokarelidic episodes, (2) the c. 2 200 m.y. Inverian episode and the c. 2 300 m.y. episode...

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Main Author: D.R. Bowes
Format: Article
Language:English
Published: Geological Society of Finland 1975-12-01
Series:Bulletin of the Geological Society of Finland
Online Access:http://www.geologinenseura.fi/bulletin/Volume47/sgs_bt_047_pages_001_012.pdf
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author D.R. Bowes
author_facet D.R. Bowes
author_sort D.R. Bowes
collection DOAJ
description Isotopic age determinations indicate the generally co-eval nature of major episodes of earth history shown by the Precambrian rocks of Scotland and Finland, viz. (1) the c. 2 800—2 600 m.y. Scourian and Presvecokarelidic episodes, (2) the c. 2 200 m.y. Inverian episode and the c. 2 300 m.y. episode in Finland, (3) the c. 2.1 b.y. deposition of the Loch Maree Group in Scotland and the Jatulian quartzite, Karelian schists and related geosynclinal deposits in Finland, and (4) the c. 1 975—1 700 m.y. Laxfordian and Svecokarelian episodes. The existence of spatially connected belts in Precambrian times is suggested by the correspondence in both the sequence of development and the orientations of structural elements resulting from polyphase deformation in the successively formed Precambrian orogenic belts. This matching of complex structural frameworks implies that, before the initiation of the British-Scandinavian Caledonides, the Baltic Shield extended westward to include northwestern Britain and the continental shelf of the eastern North Atlantic Ocean. The Caledonian belt would then have developed on a plate of continental crust, or between the separated parts of a rifted continental crustal segment.
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spelling doaj.art-cdc7db248a074794aa12b0935c8bec1e2022-12-21T20:55:31ZengGeological Society of FinlandBulletin of the Geological Society of Finland0367-52111799-46321975-12-01471-211210.17741/bgsf/47.1-2.001Scotland–Finland Precambrian correlationsD.R. BowesIsotopic age determinations indicate the generally co-eval nature of major episodes of earth history shown by the Precambrian rocks of Scotland and Finland, viz. (1) the c. 2 800—2 600 m.y. Scourian and Presvecokarelidic episodes, (2) the c. 2 200 m.y. Inverian episode and the c. 2 300 m.y. episode in Finland, (3) the c. 2.1 b.y. deposition of the Loch Maree Group in Scotland and the Jatulian quartzite, Karelian schists and related geosynclinal deposits in Finland, and (4) the c. 1 975—1 700 m.y. Laxfordian and Svecokarelian episodes. The existence of spatially connected belts in Precambrian times is suggested by the correspondence in both the sequence of development and the orientations of structural elements resulting from polyphase deformation in the successively formed Precambrian orogenic belts. This matching of complex structural frameworks implies that, before the initiation of the British-Scandinavian Caledonides, the Baltic Shield extended westward to include northwestern Britain and the continental shelf of the eastern North Atlantic Ocean. The Caledonian belt would then have developed on a plate of continental crust, or between the separated parts of a rifted continental crustal segment.http://www.geologinenseura.fi/bulletin/Volume47/sgs_bt_047_pages_001_012.pdf
spellingShingle D.R. Bowes
Scotland–Finland Precambrian correlations
Bulletin of the Geological Society of Finland
title Scotland–Finland Precambrian correlations
title_full Scotland–Finland Precambrian correlations
title_fullStr Scotland–Finland Precambrian correlations
title_full_unstemmed Scotland–Finland Precambrian correlations
title_short Scotland–Finland Precambrian correlations
title_sort scotland finland precambrian correlations
url http://www.geologinenseura.fi/bulletin/Volume47/sgs_bt_047_pages_001_012.pdf
work_keys_str_mv AT drbowes scotlandfinlandprecambriancorrelations