The geological evolution of the North Sea area in the tectonic framework of North Western Europe.
The development history of the North Sea area can be subdivided into five stages: 1) Caledonian geosynclinal stage (Cambrian-Silurian), 2) Variscan geosynclinal stage (Devoanin-Carboniferous), 3) Permo-Triassic intracratonic stage, 4) Jurassic-Cretaceous taphrogenic rifting stage, 5) Tertiary post-r...
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1975
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ftnorgesgu:oai:openarchive.ngu.no:11250/2674997 2023-05-15T15:00:16+02:00 The geological evolution of the North Sea area in the tectonic framework of North Western Europe. Ziegler, Peter A. 1975 application/pdf https://hdl.handle.net/11250/2674997 eng eng NGU (316) https://hdl.handle.net/11250/2674997 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 1-27 STRATIGRAFI BERGGRUNNSGEOLOGI TEKTONIKK Journal article 1975 ftnorgesgu 2022-07-03T15:26:39Z The development history of the North Sea area can be subdivided into five stages: 1) Caledonian geosynclinal stage (Cambrian-Silurian), 2) Variscan geosynclinal stage (Devoanin-Carboniferous), 3) Permo-Triassic intracratonic stage, 4) Jurassic-Cretaceous taphrogenic rifting stage, 5) Tertiary post-rifting intracratonic stage. The Jurassic-Cretaceous North Sea central rift system is related to the rifting processes in the Arctic North Atlantic. During the Tertiary this sector of the Atlantic entered the drifting stage. At the same time the North Sea rift system became inactive, leading to regional subsidence. Emplacement of the late Tertiary Rh\u00F4ne-Rhine rift system postdates the central North Sea rift. 35888 Article in Journal/Newspaper Arctic North Atlantic NGU Open Archive (Geological Survey of Norway) Arctic |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
English |
topic |
STRATIGRAFI BERGGRUNNSGEOLOGI TEKTONIKK |
spellingShingle |
STRATIGRAFI BERGGRUNNSGEOLOGI TEKTONIKK Ziegler, Peter A. The geological evolution of the North Sea area in the tectonic framework of North Western Europe. |
topic_facet |
STRATIGRAFI BERGGRUNNSGEOLOGI TEKTONIKK |
description |
The development history of the North Sea area can be subdivided into five stages: 1) Caledonian geosynclinal stage (Cambrian-Silurian), 2) Variscan geosynclinal stage (Devoanin-Carboniferous), 3) Permo-Triassic intracratonic stage, 4) Jurassic-Cretaceous taphrogenic rifting stage, 5) Tertiary post-rifting intracratonic stage. The Jurassic-Cretaceous North Sea central rift system is related to the rifting processes in the Arctic North Atlantic. During the Tertiary this sector of the Atlantic entered the drifting stage. At the same time the North Sea rift system became inactive, leading to regional subsidence. Emplacement of the late Tertiary Rh\u00F4ne-Rhine rift system postdates the central North Sea rift. 35888 |
format |
Article in Journal/Newspaper |
author |
Ziegler, Peter A. |
author_facet |
Ziegler, Peter A. |
author_sort |
Ziegler, Peter A. |
title |
The geological evolution of the North Sea area in the tectonic framework of North Western Europe. |
title_short |
The geological evolution of the North Sea area in the tectonic framework of North Western Europe. |
title_full |
The geological evolution of the North Sea area in the tectonic framework of North Western Europe. |
title_fullStr |
The geological evolution of the North Sea area in the tectonic framework of North Western Europe. |
title_full_unstemmed |
The geological evolution of the North Sea area in the tectonic framework of North Western Europe. |
title_sort |
geological evolution of the north sea area in the tectonic framework of north western europe. |
publishDate |
1975 |
url |
https://hdl.handle.net/11250/2674997 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic North Atlantic |
genre_facet |
Arctic North Atlantic |
op_source |
1-27 |
op_relation |
NGU (316) https://hdl.handle.net/11250/2674997 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766332369371922432 |