Gravity and Deep Structure of the Continental Margin of Banks Island and Mackenzie Delta
Regional and deep structure supported by drill hole, gravity, and seismic evidence is interpreted along five profiles—one across the Mackenzie Delta and four across the continental margin. Isostatic compensation has reduced the gravity effect of most structures but gravity anomalies are still suffic...
Published in: | Canadian Journal of Earth Sciences |
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Language: | English |
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Canadian Science Publishing
1975
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Online Access: | http://dx.doi.org/10.1139/e75-035 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-035 |
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crcansciencepubl:10.1139/e75-035 2024-09-15T17:57:34+00:00 Gravity and Deep Structure of the Continental Margin of Banks Island and Mackenzie Delta Sobczak, L. W. 1975 http://dx.doi.org/10.1139/e75-035 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-035 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 12, issue 3, page 378-394 ISSN 0008-4077 1480-3313 journal-article 1975 crcansciencepubl https://doi.org/10.1139/e75-035 2024-07-25T04:10:06Z Regional and deep structure supported by drill hole, gravity, and seismic evidence is interpreted along five profiles—one across the Mackenzie Delta and four across the continental margin. Isostatic compensation has reduced the gravity effect of most structures but gravity anomalies are still sufficient to outline two major sedimentary basins—one very extensive and thick (>10 km) underlying the continental margin and Mackenzie Delta and the other narrow and shallow east and southeast of the Arctic Coastal Plain. A basement ridge separating these basins along the eastern side of the Arctic Coastal Plain is outlined by a trend of relative gravity highs.An arcuate belt of prominent elliptically-shaped free air gravity highs (peak values >100 mgal) over the continental break outlines an uncompensated region of mass excesses. These mass excesses are explained by pro-grading wedges (>2 km thick) of Quaternary and possibly Tertiary sediments that have displaced seawater and act as a load on the crust rather than by the alternative concepts of an uncompensated ridge or high density material in the basement. Article in Journal/Newspaper Banks Island Mackenzie Delta Canadian Science Publishing Canadian Journal of Earth Sciences 12 3 378 394 |
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Open Polar |
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Canadian Science Publishing |
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crcansciencepubl |
language |
English |
description |
Regional and deep structure supported by drill hole, gravity, and seismic evidence is interpreted along five profiles—one across the Mackenzie Delta and four across the continental margin. Isostatic compensation has reduced the gravity effect of most structures but gravity anomalies are still sufficient to outline two major sedimentary basins—one very extensive and thick (>10 km) underlying the continental margin and Mackenzie Delta and the other narrow and shallow east and southeast of the Arctic Coastal Plain. A basement ridge separating these basins along the eastern side of the Arctic Coastal Plain is outlined by a trend of relative gravity highs.An arcuate belt of prominent elliptically-shaped free air gravity highs (peak values >100 mgal) over the continental break outlines an uncompensated region of mass excesses. These mass excesses are explained by pro-grading wedges (>2 km thick) of Quaternary and possibly Tertiary sediments that have displaced seawater and act as a load on the crust rather than by the alternative concepts of an uncompensated ridge or high density material in the basement. |
format |
Article in Journal/Newspaper |
author |
Sobczak, L. W. |
spellingShingle |
Sobczak, L. W. Gravity and Deep Structure of the Continental Margin of Banks Island and Mackenzie Delta |
author_facet |
Sobczak, L. W. |
author_sort |
Sobczak, L. W. |
title |
Gravity and Deep Structure of the Continental Margin of Banks Island and Mackenzie Delta |
title_short |
Gravity and Deep Structure of the Continental Margin of Banks Island and Mackenzie Delta |
title_full |
Gravity and Deep Structure of the Continental Margin of Banks Island and Mackenzie Delta |
title_fullStr |
Gravity and Deep Structure of the Continental Margin of Banks Island and Mackenzie Delta |
title_full_unstemmed |
Gravity and Deep Structure of the Continental Margin of Banks Island and Mackenzie Delta |
title_sort |
gravity and deep structure of the continental margin of banks island and mackenzie delta |
publisher |
Canadian Science Publishing |
publishDate |
1975 |
url |
http://dx.doi.org/10.1139/e75-035 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-035 |
genre |
Banks Island Mackenzie Delta |
genre_facet |
Banks Island Mackenzie Delta |
op_source |
Canadian Journal of Earth Sciences volume 12, issue 3, page 378-394 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e75-035 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
12 |
container_issue |
3 |
container_start_page |
378 |
op_container_end_page |
394 |
_version_ |
1810433695879790592 |