A geological case for movement between Canada and Greenland along Nares Strait
Nares Strait, part of a 1400 km long lineament between Canada and Greenland, may be one arm (along with Lancaster Sound and Baffin Bay) of a triple junction. Study of the geological literature on the area from northern Baffin Island to northern Greenland revealed a number of possibly important marke...
Published in: | Meddelelser om Grønland. Geoscience |
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Language: | English |
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The Commission for Scientific Research in Greenland /Danish Polar Center
1982
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Online Access: | https://tidsskrift.dk/meddrgroenland_geosci/article/view/141059 |
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ftsbaarhusojs:oai:ojs.tidsskrift.dk:article/141059 2024-01-28T10:04:38+01:00 A geological case for movement between Canada and Greenland along Nares Strait H. Newman, Patricia 1982-06-10 application/pdf https://tidsskrift.dk/meddrgroenland_geosci/article/view/141059 eng eng The Commission for Scientific Research in Greenland /Danish Polar Center https://tidsskrift.dk/meddrgroenland_geosci/article/view/141059/184946 https://tidsskrift.dk/meddrgroenland_geosci/article/view/141059 Meddelelser om Grønland. Geoscience; Vol. 8 (1982): Meddelelser om Grønland. Geoscience; 199–204 Meddelelser om Grønland. Geoscience; Årg. 8 (1982): Meddelelser om Grønland, Geoscience; 199–204 1600-4590 0106-1046 10.7146/moggeosci.v8i info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1982 ftsbaarhusojs https://doi.org/10.7146/moggeosci.v8i 2024-01-03T23:59:20Z Nares Strait, part of a 1400 km long lineament between Canada and Greenland, may be one arm (along with Lancaster Sound and Baffin Bay) of a triple junction. Study of the geological literature on the area from northern Baffin Island to northern Greenland revealed a number of possibly important markers and structural features. The most important of these are: 1) the structural boundary between deformed and undeformed rocks at the margin of the Palaeozoic fold belt of northern Ellesmere Island and Greenland and 2) the large asymmetrical northwest-trending graben systems of northern Baffin Island and Greenland, whose fault blocks tilt to the northeast and southwest respectively. Correlation of these features across Nares Strait suggests that movement along the Strait of a minimum of 200 km has occurred since the mid-Palaeozoic, and a maximum of 300 km since late Precambrian times. It seems probable that the movement occurred in a number of episodes, beginning with rifting in the Proterozoic and ending in the Tertiary Eurekan orogeny. Article in Journal/Newspaper Baffin Bay Baffin Bay Baffin Island Baffin Ellesmere Island Greenland Lancaster Sound Nares strait Aarhus University: OJS at The State and University Library Baffin Bay Baffin Island Ellesmere Island Canada Greenland Lancaster Sound ENVELOPE(-83.999,-83.999,74.218,74.218) Nares ENVELOPE(158.167,158.167,-81.450,-81.450) Meddelelser om Grønland. Geoscience 8 |
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Open Polar |
collection |
Aarhus University: OJS at The State and University Library |
op_collection_id |
ftsbaarhusojs |
language |
English |
description |
Nares Strait, part of a 1400 km long lineament between Canada and Greenland, may be one arm (along with Lancaster Sound and Baffin Bay) of a triple junction. Study of the geological literature on the area from northern Baffin Island to northern Greenland revealed a number of possibly important markers and structural features. The most important of these are: 1) the structural boundary between deformed and undeformed rocks at the margin of the Palaeozoic fold belt of northern Ellesmere Island and Greenland and 2) the large asymmetrical northwest-trending graben systems of northern Baffin Island and Greenland, whose fault blocks tilt to the northeast and southwest respectively. Correlation of these features across Nares Strait suggests that movement along the Strait of a minimum of 200 km has occurred since the mid-Palaeozoic, and a maximum of 300 km since late Precambrian times. It seems probable that the movement occurred in a number of episodes, beginning with rifting in the Proterozoic and ending in the Tertiary Eurekan orogeny. |
format |
Article in Journal/Newspaper |
author |
H. Newman, Patricia |
spellingShingle |
H. Newman, Patricia A geological case for movement between Canada and Greenland along Nares Strait |
author_facet |
H. Newman, Patricia |
author_sort |
H. Newman, Patricia |
title |
A geological case for movement between Canada and Greenland along Nares Strait |
title_short |
A geological case for movement between Canada and Greenland along Nares Strait |
title_full |
A geological case for movement between Canada and Greenland along Nares Strait |
title_fullStr |
A geological case for movement between Canada and Greenland along Nares Strait |
title_full_unstemmed |
A geological case for movement between Canada and Greenland along Nares Strait |
title_sort |
geological case for movement between canada and greenland along nares strait |
publisher |
The Commission for Scientific Research in Greenland /Danish Polar Center |
publishDate |
1982 |
url |
https://tidsskrift.dk/meddrgroenland_geosci/article/view/141059 |
long_lat |
ENVELOPE(-83.999,-83.999,74.218,74.218) ENVELOPE(158.167,158.167,-81.450,-81.450) |
geographic |
Baffin Bay Baffin Island Ellesmere Island Canada Greenland Lancaster Sound Nares |
geographic_facet |
Baffin Bay Baffin Island Ellesmere Island Canada Greenland Lancaster Sound Nares |
genre |
Baffin Bay Baffin Bay Baffin Island Baffin Ellesmere Island Greenland Lancaster Sound Nares strait |
genre_facet |
Baffin Bay Baffin Bay Baffin Island Baffin Ellesmere Island Greenland Lancaster Sound Nares strait |
op_source |
Meddelelser om Grønland. Geoscience; Vol. 8 (1982): Meddelelser om Grønland. Geoscience; 199–204 Meddelelser om Grønland. Geoscience; Årg. 8 (1982): Meddelelser om Grønland, Geoscience; 199–204 1600-4590 0106-1046 10.7146/moggeosci.v8i |
op_relation |
https://tidsskrift.dk/meddrgroenland_geosci/article/view/141059/184946 https://tidsskrift.dk/meddrgroenland_geosci/article/view/141059 |
op_doi |
https://doi.org/10.7146/moggeosci.v8i |
container_title |
Meddelelser om Grønland. Geoscience |
container_volume |
8 |
_version_ |
1789330411542806528 |