The Norwegian Margin formed in response to early Cenozoic continental breakup and subsequent opening of the Norwegian-Greenland Sea. There is a well-defined margin segmentation and the various segments are characterized by distinct crustal properties, struc-tural and magmatic styles, and post-openin...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.475.9034 http://www.episodes.co.in/www/backissues/33igc/13r.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.475.9034 2023-05-15T15:38:41+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.475.9034 http://www.episodes.co.in/www/backissues/33igc/13r.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.475.9034 http://www.episodes.co.in/www/backissues/33igc/13r.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.episodes.co.in/www/backissues/33igc/13r.pdf text ftciteseerx 2016-01-08T07:35:12Z The Norwegian Margin formed in response to early Cenozoic continental breakup and subsequent opening of the Norwegian-Greenland Sea. There is a well-defined margin segmentation and the various segments are characterized by distinct crustal properties, struc-tural and magmatic styles, and post-opening history of vertical motions. The sedimentary basins at the conju-gate continental margins off Norway and Greenland and in the western Barents Sea developed as a result of a series of post-Caledonian rift episodes until early Cenozoic time, when complete continental separation took place. Text Barents Sea Greenland Greenland Sea Unknown Barents Sea Greenland Norway |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
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The Norwegian Margin formed in response to early Cenozoic continental breakup and subsequent opening of the Norwegian-Greenland Sea. There is a well-defined margin segmentation and the various segments are characterized by distinct crustal properties, struc-tural and magmatic styles, and post-opening history of vertical motions. The sedimentary basins at the conju-gate continental margins off Norway and Greenland and in the western Barents Sea developed as a result of a series of post-Caledonian rift episodes until early Cenozoic time, when complete continental separation took place. |
| author2 |
The Pennsylvania State University CiteSeerX Archives |
| format |
Text |
| url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.475.9034 http://www.episodes.co.in/www/backissues/33igc/13r.pdf |
| geographic |
Barents Sea Greenland Norway |
| geographic_facet |
Barents Sea Greenland Norway |
| genre |
Barents Sea Greenland Greenland Sea |
| genre_facet |
Barents Sea Greenland Greenland Sea |
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http://www.episodes.co.in/www/backissues/33igc/13r.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.475.9034 http://www.episodes.co.in/www/backissues/33igc/13r.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766369921284964352 |