Crustal structure and velocity anisotropy beneath the Beaufort Sea
Crustal-scale seismic refraction data obtained in the Beaufort Sea during 1976 reveal a 4–5 km thick sedimentary layer overlying an oceanic crust that thickens rapidly as it approaches the continental terrace of Alaska. A synthetic seismogram analysis of multiple reflected, water-wave events indicat...
Published in: | Canadian Journal of Earth Sciences |
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Canadian Science Publishing
1981
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Online Access: | http://dx.doi.org/10.1139/e81-067 http://www.nrcresearchpress.com/doi/pdf/10.1139/e81-067 |
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crcansciencepubl:10.1139/e81-067 2024-09-15T17:58:14+00:00 Crustal structure and velocity anisotropy beneath the Beaufort Sea Mair, J. A. Lyons, J. A. 1981 http://dx.doi.org/10.1139/e81-067 http://www.nrcresearchpress.com/doi/pdf/10.1139/e81-067 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 18, issue 4, page 724-741 ISSN 0008-4077 1480-3313 journal-article 1981 crcansciencepubl https://doi.org/10.1139/e81-067 2024-08-01T04:10:01Z Crustal-scale seismic refraction data obtained in the Beaufort Sea during 1976 reveal a 4–5 km thick sedimentary layer overlying an oceanic crust that thickens rapidly as it approaches the continental terrace of Alaska. A synthetic seismogram analysis of multiple reflected, water-wave events indicates that the upper sedimentary layer has a compressional velocity of 1.8 km/s and a shear velocity of about 0.2 km/s. An oceanic layer 2A of 4.3 km/s, a layer 3A of 6.6 km/s, and a layer 3B of 7.6 km/s overlying an anisotropic (3%) upper mantle with a median velocity of 8.3 km/s are interpreted. The direction of maximum upper-mantle velocity appears to be approximately north–south in the area surveyed, suggesting that a rotation of the Northwind Ridge–Chukchi Plateau away from the Barrow–Martin Point sector of Alaska may have occurred. Article in Journal/Newspaper Barrow Beaufort Sea Chukchi Alaska Canadian Science Publishing Canadian Journal of Earth Sciences 18 4 724 741 |
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Open Polar |
collection |
Canadian Science Publishing |
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crcansciencepubl |
language |
English |
description |
Crustal-scale seismic refraction data obtained in the Beaufort Sea during 1976 reveal a 4–5 km thick sedimentary layer overlying an oceanic crust that thickens rapidly as it approaches the continental terrace of Alaska. A synthetic seismogram analysis of multiple reflected, water-wave events indicates that the upper sedimentary layer has a compressional velocity of 1.8 km/s and a shear velocity of about 0.2 km/s. An oceanic layer 2A of 4.3 km/s, a layer 3A of 6.6 km/s, and a layer 3B of 7.6 km/s overlying an anisotropic (3%) upper mantle with a median velocity of 8.3 km/s are interpreted. The direction of maximum upper-mantle velocity appears to be approximately north–south in the area surveyed, suggesting that a rotation of the Northwind Ridge–Chukchi Plateau away from the Barrow–Martin Point sector of Alaska may have occurred. |
format |
Article in Journal/Newspaper |
author |
Mair, J. A. Lyons, J. A. |
spellingShingle |
Mair, J. A. Lyons, J. A. Crustal structure and velocity anisotropy beneath the Beaufort Sea |
author_facet |
Mair, J. A. Lyons, J. A. |
author_sort |
Mair, J. A. |
title |
Crustal structure and velocity anisotropy beneath the Beaufort Sea |
title_short |
Crustal structure and velocity anisotropy beneath the Beaufort Sea |
title_full |
Crustal structure and velocity anisotropy beneath the Beaufort Sea |
title_fullStr |
Crustal structure and velocity anisotropy beneath the Beaufort Sea |
title_full_unstemmed |
Crustal structure and velocity anisotropy beneath the Beaufort Sea |
title_sort |
crustal structure and velocity anisotropy beneath the beaufort sea |
publisher |
Canadian Science Publishing |
publishDate |
1981 |
url |
http://dx.doi.org/10.1139/e81-067 http://www.nrcresearchpress.com/doi/pdf/10.1139/e81-067 |
genre |
Barrow Beaufort Sea Chukchi Alaska |
genre_facet |
Barrow Beaufort Sea Chukchi Alaska |
op_source |
Canadian Journal of Earth Sciences volume 18, issue 4, page 724-741 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e81-067 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
18 |
container_issue |
4 |
container_start_page |
724 |
op_container_end_page |
741 |
_version_ |
1810434626938732544 |