By Knut S. Heier (auth.), A. M. Spencer (eds.)
ISBN-10: 9400956266
ISBN-13: 9789400956261
ISBN-10: 9401089825
ISBN-13: 9789401089821
Read Online or Download Petroleum Geology of the North European Margin: Proceedings of the North European Margin Symposium (NEMS ’83), organized by the Norwegian Petroleum Society and held at the Norwegian Institute of Technology (NTH) in Trondheim 9–11 May, 1983 PDF
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Extra info for Petroleum Geology of the North European Margin: Proceedings of the North European Margin Symposium (NEMS ’83), organized by the Norwegian Petroleum Society and held at the Norwegian Institute of Technology (NTH) in Trondheim 9–11 May, 1983
Sample text
Nomenclature for Structural Features Description Nordland Ridge (Nordlandryggen) On the Norwegian mainland, the Me/>re-Tre/>ndelag Fault Zone affects Precambrian and, in part, Caledonian rocks which are dominated by an ENE-WSW structural grain. This zone includes some of the major faults known in the area, such as the Beistadfjorden Fault, the Tarva Fault, the Hitra Fault and the Verran Fault (Oftedahl, 1972, 1975). Most of the faults are normal, although Aanstad et aZ. (1981) described field evidence for small-scale strike-slip movements.
Most of the faults are normal, although Aanstad et aZ. (1981) described field evidence for small-scale strike-slip movements. This structural trend continues offshore where it delimits major structural elements such as the Tre/>ndelag Platform, the Horda Platform and the Me/>re Basin. Named after Nordland County. Age The ENE-WSW structural grain in the northwestern part of Norway can be related to the Caledonian deformations. , 1968; Raheim 1974). In off-shore areas Price and Rattey (in press) have suggested dextral transcurrent movements on the ENE-WSW system in Cretaceous time, which altogether suggest a long-lived tectonic activity along the Me/>re-Tre/>ndelag Fault Zone.
Over the topographically highest part of the V~ring Plateau, the basement has a thin Tertiary cover. In the southeast the basement dips steeply to the southeast and becomes buried below the thick sedimentary sequence in the V ~ring Basin. The inner part (which is identical to the V~ring Basin) is subdivided into two basinal elements (Sm~la Rift and R~st Sub-basin). Age The V~ring Plateau is a structural feature which is related to the Tertiary opening of the North Atlantic. However, this area may also have existed as a structural high in Cretaceous and even preCretaceous time, when the V~ring Basin developed.
Petroleum Geology of the North European Margin: Proceedings of the North European Margin Symposium (NEMS ’83), organized by the Norwegian Petroleum Society and held at the Norwegian Institute of Technology (NTH) in Trondheim 9–11 May, 1983 by Knut S. Heier (auth.), A. M. Spencer (eds.)
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