Paleomagnetism of the Circum-Ungava Proterozoic Fold Belt (I): Cape Smith Komatiitic Basalts
A total of 397 oriented cores were taken from pillowed, columnar, and massive basalt of Cape Smith Island in northeastern Hudson Bay and from the adjacent mainland coast of Quebec. The thick series of basalts form part of the Circum-Ungava Proterozoic Belt which is of Aphebian (early Proterozoic) ag...
Published in: | Canadian Journal of Earth Sciences |
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Canadian Science Publishing
1975
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Online Access: | http://dx.doi.org/10.1139/e75-158 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-158 |
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crcansciencepubl:10.1139/e75-158 2023-12-17T10:31:24+01:00 Paleomagnetism of the Circum-Ungava Proterozoic Fold Belt (I): Cape Smith Komatiitic Basalts Fujiwara, Y. Schwarz, E. J. 1975 http://dx.doi.org/10.1139/e75-158 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-158 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 12, issue 10, page 1785-1793 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1975 crcansciencepubl https://doi.org/10.1139/e75-158 2023-11-19T13:39:35Z A total of 397 oriented cores were taken from pillowed, columnar, and massive basalt of Cape Smith Island in northeastern Hudson Bay and from the adjacent mainland coast of Quebec. The thick series of basalts form part of the Circum-Ungava Proterozoic Belt which is of Aphebian (early Proterozoic) age. The lower portion of the basalt series contains pyrrhotite (Fe 7 S 8 ) and did not yield useful paleomagnetic results. The magnetization of the upper portion of the series is carried by small quantities [Formula: see text] of magnetite. The directions of magnetization of the samples do not change much during alternating field and thermal washing, and show very good grouping. The available internal evidence on the age of the stable remanence is inconclusive. The pole position (20°N, 162°E, semi-axes of the 95% oval of confidence: 4 °and 5°) after correcting for tilt is about 70° west of the preHudsonian part of the polar wandering curve established from North American data. The uncorrected pole position (16°N, 107°W), which would apply if the magnetization was acquired at the time of the Hudsonian orogeny, is in the general area of paleomagnetic poles for rocks of similar age from other localities of the Canadian Shield. Article in Journal/Newspaper Hudson Bay Smith Island Canadian Science Publishing (via Crossref) Hudson Bay Hudson Smith Island ENVELOPE(-62.520,-62.520,-62.981,-62.981) Cape Smith ENVELOPE(-62.520,-62.520,-62.981,-62.981) Canadian Journal of Earth Sciences 12 10 1785 1793 |
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 Fujiwara, Y. Schwarz, E. J. Paleomagnetism of the Circum-Ungava Proterozoic Fold Belt (I): Cape Smith Komatiitic Basalts |
topic_facet |
General Earth and Planetary Sciences |
description |
A total of 397 oriented cores were taken from pillowed, columnar, and massive basalt of Cape Smith Island in northeastern Hudson Bay and from the adjacent mainland coast of Quebec. The thick series of basalts form part of the Circum-Ungava Proterozoic Belt which is of Aphebian (early Proterozoic) age. The lower portion of the basalt series contains pyrrhotite (Fe 7 S 8 ) and did not yield useful paleomagnetic results. The magnetization of the upper portion of the series is carried by small quantities [Formula: see text] of magnetite. The directions of magnetization of the samples do not change much during alternating field and thermal washing, and show very good grouping. The available internal evidence on the age of the stable remanence is inconclusive. The pole position (20°N, 162°E, semi-axes of the 95% oval of confidence: 4 °and 5°) after correcting for tilt is about 70° west of the preHudsonian part of the polar wandering curve established from North American data. The uncorrected pole position (16°N, 107°W), which would apply if the magnetization was acquired at the time of the Hudsonian orogeny, is in the general area of paleomagnetic poles for rocks of similar age from other localities of the Canadian Shield. |
format |
Article in Journal/Newspaper |
author |
Fujiwara, Y. Schwarz, E. J. |
author_facet |
Fujiwara, Y. Schwarz, E. J. |
author_sort |
Fujiwara, Y. |
title |
Paleomagnetism of the Circum-Ungava Proterozoic Fold Belt (I): Cape Smith Komatiitic Basalts |
title_short |
Paleomagnetism of the Circum-Ungava Proterozoic Fold Belt (I): Cape Smith Komatiitic Basalts |
title_full |
Paleomagnetism of the Circum-Ungava Proterozoic Fold Belt (I): Cape Smith Komatiitic Basalts |
title_fullStr |
Paleomagnetism of the Circum-Ungava Proterozoic Fold Belt (I): Cape Smith Komatiitic Basalts |
title_full_unstemmed |
Paleomagnetism of the Circum-Ungava Proterozoic Fold Belt (I): Cape Smith Komatiitic Basalts |
title_sort |
paleomagnetism of the circum-ungava proterozoic fold belt (i): cape smith komatiitic basalts |
publisher |
Canadian Science Publishing |
publishDate |
1975 |
url |
http://dx.doi.org/10.1139/e75-158 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-158 |
long_lat |
ENVELOPE(-62.520,-62.520,-62.981,-62.981) ENVELOPE(-62.520,-62.520,-62.981,-62.981) |
geographic |
Hudson Bay Hudson Smith Island Cape Smith |
geographic_facet |
Hudson Bay Hudson Smith Island Cape Smith |
genre |
Hudson Bay Smith Island |
genre_facet |
Hudson Bay Smith Island |
op_source |
Canadian Journal of Earth Sciences volume 12, issue 10, page 1785-1793 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e75-158 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
12 |
container_issue |
10 |
container_start_page |
1785 |
op_container_end_page |
1793 |
_version_ |
1785584698696663040 |