Metamorphosed and deformed pillows from Losomäki: evidence of sub-aqueous volcanism in the Outokumpu association, eastern Finland

Pillow lavas, some highly deformed and now seen as banded diopside amphibolites and tremolite-epidote-chlorite rocks (»barren skarn»), occur within the lower Proterozoic Outokumpu rock association at Losomäki, 50 km N.W. of Outokumpu. The occurrence of these sub-aqueous volcanic assemblages, togethe...

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Main Authors: A.F. Park, D.R. Bowes
Format: Article
Language:English
Published: Geological Society of Finland 1981-12-01
Series:Bulletin of the Geological Society of Finland
Online Access:http://www.geologinenseura.fi/bulletin/Volume53/sgs_bt_053_2_pages_135_145.pdf
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author A.F. Park
D.R. Bowes
author_facet A.F. Park
D.R. Bowes
author_sort A.F. Park
collection DOAJ
description Pillow lavas, some highly deformed and now seen as banded diopside amphibolites and tremolite-epidote-chlorite rocks (»barren skarn»), occur within the lower Proterozoic Outokumpu rock association at Losomäki, 50 km N.W. of Outokumpu. The occurrence of these sub-aqueous volcanic assemblages, together with the previously described serpentinite—metadolomite—non-detrital quartzite—cupriferous sulphide ore—black schist assemblage, is similar to those found in both Phanerozoic ophiolite complexes and the lower members of Archaean greenstone belts. The nature of this assemblage is of significance in assessing the lithospheric processes operative in early Proterozoic times as well as in elucidating the evolution of the Svecokarelides.
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spelling doaj.art-81200d129b97450c8a981468052b22bc2022-12-21T19:08:06ZengGeological Society of FinlandBulletin of the Geological Society of Finland0367-52111799-46321981-12-0153213514510.17741/bgsf/53.2.006Metamorphosed and deformed pillows from Losomäki: evidence of sub-aqueous volcanism in the Outokumpu association, eastern FinlandA.F. ParkD.R. BowesPillow lavas, some highly deformed and now seen as banded diopside amphibolites and tremolite-epidote-chlorite rocks (»barren skarn»), occur within the lower Proterozoic Outokumpu rock association at Losomäki, 50 km N.W. of Outokumpu. The occurrence of these sub-aqueous volcanic assemblages, together with the previously described serpentinite—metadolomite—non-detrital quartzite—cupriferous sulphide ore—black schist assemblage, is similar to those found in both Phanerozoic ophiolite complexes and the lower members of Archaean greenstone belts. The nature of this assemblage is of significance in assessing the lithospheric processes operative in early Proterozoic times as well as in elucidating the evolution of the Svecokarelides.http://www.geologinenseura.fi/bulletin/Volume53/sgs_bt_053_2_pages_135_145.pdf
spellingShingle A.F. Park
D.R. Bowes
Metamorphosed and deformed pillows from Losomäki: evidence of sub-aqueous volcanism in the Outokumpu association, eastern Finland
Bulletin of the Geological Society of Finland
title Metamorphosed and deformed pillows from Losomäki: evidence of sub-aqueous volcanism in the Outokumpu association, eastern Finland
title_full Metamorphosed and deformed pillows from Losomäki: evidence of sub-aqueous volcanism in the Outokumpu association, eastern Finland
title_fullStr Metamorphosed and deformed pillows from Losomäki: evidence of sub-aqueous volcanism in the Outokumpu association, eastern Finland
title_full_unstemmed Metamorphosed and deformed pillows from Losomäki: evidence of sub-aqueous volcanism in the Outokumpu association, eastern Finland
title_short Metamorphosed and deformed pillows from Losomäki: evidence of sub-aqueous volcanism in the Outokumpu association, eastern Finland
title_sort metamorphosed and deformed pillows from losomaki evidence of sub aqueous volcanism in the outokumpu association eastern finland
url http://www.geologinenseura.fi/bulletin/Volume53/sgs_bt_053_2_pages_135_145.pdf
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