Paleomagnetic reexamination of the Lower Ordovician Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland
The Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland contain oolitic hematite beds of Early Ordovician age, dipping ~11° north-northwest. Twenty-one oolitic hematite samples from nine sites were thermally demagnetized in 10 or 11 steps to 660 or 680 °C. At 450 °C, 15 samples fro...
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Language: | English |
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Canadian Science Publishing
1982
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Online Access: | http://dx.doi.org/10.1139/e82-087 http://www.nrcresearchpress.com/doi/pdf/10.1139/e82-087 |
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crcansciencepubl:10.1139/e82-087 2024-06-23T07:51:41+00:00 Paleomagnetic reexamination of the Lower Ordovician Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland Buchan, K. L. Hodych, J. P. 1982 http://dx.doi.org/10.1139/e82-087 http://www.nrcresearchpress.com/doi/pdf/10.1139/e82-087 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 19, issue 5, page 1055-1069 ISSN 0008-4077 1480-3313 journal-article 1982 crcansciencepubl https://doi.org/10.1139/e82-087 2024-06-06T04:11:16Z The Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland contain oolitic hematite beds of Early Ordovician age, dipping ~11° north-northwest. Twenty-one oolitic hematite samples from nine sites were thermally demagnetized in 10 or 11 steps to 660 or 680 °C. At 450 °C, 15 samples from six sites define a stable magnetization direction (D = 21.2°, I = −12.5°, k = 137, α 95 = 5.7°) with respect to bedding. The remaining six samples failed to attain the stable end-point, five of them because of growth of much "magnetite," which probably resulted from breakdown of siderite during thermal demagnetization.The paleopole for the Wabana – Bell Island Groups lies at 33°N 102°E (dm = 5.8°, dp = 3.0°). It is compared with other early Paleozoic paleopoles from cratonic North America and the Avalon zone, and its significance for the Iapetus Ocean is discussed. Article in Journal/Newspaper Bell Island Newfoundland Canadian Science Publishing Bell Island ENVELOPE(-61.967,-61.967,-64.267,-64.267) Canadian Journal of Earth Sciences 19 5 1055 1069 |
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Open Polar |
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Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
description |
The Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland contain oolitic hematite beds of Early Ordovician age, dipping ~11° north-northwest. Twenty-one oolitic hematite samples from nine sites were thermally demagnetized in 10 or 11 steps to 660 or 680 °C. At 450 °C, 15 samples from six sites define a stable magnetization direction (D = 21.2°, I = −12.5°, k = 137, α 95 = 5.7°) with respect to bedding. The remaining six samples failed to attain the stable end-point, five of them because of growth of much "magnetite," which probably resulted from breakdown of siderite during thermal demagnetization.The paleopole for the Wabana – Bell Island Groups lies at 33°N 102°E (dm = 5.8°, dp = 3.0°). It is compared with other early Paleozoic paleopoles from cratonic North America and the Avalon zone, and its significance for the Iapetus Ocean is discussed. |
format |
Article in Journal/Newspaper |
author |
Buchan, K. L. Hodych, J. P. |
spellingShingle |
Buchan, K. L. Hodych, J. P. Paleomagnetic reexamination of the Lower Ordovician Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland |
author_facet |
Buchan, K. L. Hodych, J. P. |
author_sort |
Buchan, K. L. |
title |
Paleomagnetic reexamination of the Lower Ordovician Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland |
title_short |
Paleomagnetic reexamination of the Lower Ordovician Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland |
title_full |
Paleomagnetic reexamination of the Lower Ordovician Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland |
title_fullStr |
Paleomagnetic reexamination of the Lower Ordovician Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland |
title_full_unstemmed |
Paleomagnetic reexamination of the Lower Ordovician Wabana and Bell Island Groups of the Avalon Peninsula of Newfoundland |
title_sort |
paleomagnetic reexamination of the lower ordovician wabana and bell island groups of the avalon peninsula of newfoundland |
publisher |
Canadian Science Publishing |
publishDate |
1982 |
url |
http://dx.doi.org/10.1139/e82-087 http://www.nrcresearchpress.com/doi/pdf/10.1139/e82-087 |
long_lat |
ENVELOPE(-61.967,-61.967,-64.267,-64.267) |
geographic |
Bell Island |
geographic_facet |
Bell Island |
genre |
Bell Island Newfoundland |
genre_facet |
Bell Island Newfoundland |
op_source |
Canadian Journal of Earth Sciences volume 19, issue 5, page 1055-1069 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e82-087 |
container_title |
Canadian Journal of Earth Sciences |
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19 |
container_issue |
5 |
container_start_page |
1055 |
op_container_end_page |
1069 |
_version_ |
1802642800541433856 |