Structural evolution of a section along the base of the St. Anthony Complex, northwest Newfoundland
The basal portion of the St. Anthony Complex is made up of structural slices 10–30 m thick, with unknown amounts of relative movement between them. The lowest rocks are variably deformed pillow lavas and related rocks with one pervasive foliation. These rocks are overlain by greenschists, phyllonite...
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Language: | English |
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Canadian Science Publishing
1983
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Online Access: | http://dx.doi.org/10.1139/e83-161 http://www.nrcresearchpress.com/doi/pdf/10.1139/e83-161 |
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crcansciencepubl:10.1139/e83-161 2023-12-17T10:44:54+01:00 Structural evolution of a section along the base of the St. Anthony Complex, northwest Newfoundland Craw, D. 1983 http://dx.doi.org/10.1139/e83-161 http://www.nrcresearchpress.com/doi/pdf/10.1139/e83-161 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 20, issue 11, page 1713-1724 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1983 crcansciencepubl https://doi.org/10.1139/e83-161 2023-11-19T13:38:47Z The basal portion of the St. Anthony Complex is made up of structural slices 10–30 m thick, with unknown amounts of relative movement between them. The lowest rocks are variably deformed pillow lavas and related rocks with one pervasive foliation. These rocks are overlain by greenschists, phyllonites, and mylonites with up to three planar structural elements developed. At least one of these latter surfaces (the earliest) had formed before the schists were thrust over the underlying pillow lavas. The overthrusting event resulted in deformation of underlying pillow lavas. All deformation occurred under lower greenschist facies conditions. Fold axes in the least deformed rocks have variable orientations, and this variation decreases up-section until axes are parallel and plunge gently eastwards, parallel to the stretching lineation. Parallelism between fold axes and stretching lineation implies rotation of fold axes during progressive deformation and is consistent with the rocks being part of a high-strain zone developed during regional overthrusting from east to west. Article in Journal/Newspaper Newfoundland Canadian Science Publishing (via Crossref) St. Anthony ENVELOPE(-55.597,-55.597,51.370,51.370) Canadian Journal of Earth Sciences 20 11 1713 1724 |
institution |
Open Polar |
collection |
Canadian Science Publishing (via Crossref) |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Craw, D. Structural evolution of a section along the base of the St. Anthony Complex, northwest Newfoundland |
topic_facet |
General Earth and Planetary Sciences |
description |
The basal portion of the St. Anthony Complex is made up of structural slices 10–30 m thick, with unknown amounts of relative movement between them. The lowest rocks are variably deformed pillow lavas and related rocks with one pervasive foliation. These rocks are overlain by greenschists, phyllonites, and mylonites with up to three planar structural elements developed. At least one of these latter surfaces (the earliest) had formed before the schists were thrust over the underlying pillow lavas. The overthrusting event resulted in deformation of underlying pillow lavas. All deformation occurred under lower greenschist facies conditions. Fold axes in the least deformed rocks have variable orientations, and this variation decreases up-section until axes are parallel and plunge gently eastwards, parallel to the stretching lineation. Parallelism between fold axes and stretching lineation implies rotation of fold axes during progressive deformation and is consistent with the rocks being part of a high-strain zone developed during regional overthrusting from east to west. |
format |
Article in Journal/Newspaper |
author |
Craw, D. |
author_facet |
Craw, D. |
author_sort |
Craw, D. |
title |
Structural evolution of a section along the base of the St. Anthony Complex, northwest Newfoundland |
title_short |
Structural evolution of a section along the base of the St. Anthony Complex, northwest Newfoundland |
title_full |
Structural evolution of a section along the base of the St. Anthony Complex, northwest Newfoundland |
title_fullStr |
Structural evolution of a section along the base of the St. Anthony Complex, northwest Newfoundland |
title_full_unstemmed |
Structural evolution of a section along the base of the St. Anthony Complex, northwest Newfoundland |
title_sort |
structural evolution of a section along the base of the st. anthony complex, northwest newfoundland |
publisher |
Canadian Science Publishing |
publishDate |
1983 |
url |
http://dx.doi.org/10.1139/e83-161 http://www.nrcresearchpress.com/doi/pdf/10.1139/e83-161 |
long_lat |
ENVELOPE(-55.597,-55.597,51.370,51.370) |
geographic |
St. Anthony |
geographic_facet |
St. Anthony |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_source |
Canadian Journal of Earth Sciences volume 20, issue 11, page 1713-1724 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e83-161 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
20 |
container_issue |
11 |
container_start_page |
1713 |
op_container_end_page |
1724 |
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1785564426185736192 |