By Knut S. Heier (auth.), A. M. Spencer (eds.)
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
A small, narrow valley created within a major fault zone by relative depression of narrow slices, or a large graben situated between tilted block movements, or a valley produced by relative uplift on opposite sides of two parallel reverse faults. Escarpment (Brattkant): A long, more or less continuous cliff or relatively steep slope facing in one general direction, breaking the continuity of an area by separating two levels or gently sloping surfaces. The escarpment is produced by erosion or by faulting.
Description The Gre/>ne/>y High is an elongated NE-trending elevation. The high is a part of the Nordland Ridge of the Kristiansund-Bode/> Fault Complex. Age The structure was initiated by early Mesozoic tectonic movements and has been reactivated as recently as late Tertiary (Miocene). In large parts of this high, late Jurassic to early Cretaceous and Miocene sediments are lacking. RcPdcPY High (RcPdcPyhcPyden) Named after a minor island off the coast of Nordland. References This structural element is defined by Gowers and Lunde (1984), and Larsen and Skarpnes (1984).
Two-way time in seconds. 28 Petroleum Geology of The North European Margin LINE 3430 - 79 s . 0 ~ ;:: .... 0 G a: .... 0 150km I I Fig. 14. Geoseismic section of Barents Sea, line 3430-79 (see Fig. 1 for location) showing the Sentralbank High, bounded by reverse faults. 0 . 2QOkm 100km 3DOkm 500km 400km Fig. 15. Geoseismic section of Barents Sea, line 7520-79 (see Fig. 1 for location). 0 50km 100km . 150km 200k", ! 25Ok", ''''m 350km I 450km I . . m Fig. 16. Geoseismic section of Barents Sea, line D-1l-79 (see Fig.