By T. P. Harding (auth.), J. P. H. Kaasschieter, T. J. A. Reijers (eds.)
ISBN-10: 9400955324
ISBN-13: 9789400955325
ISBN-10: 9401089426
ISBN-13: 9789401089425
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Additional resources for Petroleum Geology of the Southeastern North Sea and the Adjacent Onshore Areas: (The Hague, 1982)
Example text
However, seismic mapping indicates Triassic rocks extending into the area, and well data in the transition zone between the Graben and the Vestland Arch show hundreds of meters of Triassic rocks (Fig. 5d). Concerning the formation of the Graben, the lack of data allows for different interpretations. One possibility is that the Central Graben was developing in Permo-Triassic times along the NW-trending faults. The other possibility is that the Triassic north-south trend extended south into the Central Graben area and initiated the first transection of the RingkQlbing-Fyn High.
In: The sedimentation of the North Sea reservoir rocks - Norwegian Petroleum Society: 11 pp. R0nnevik, H. C .. W. van den Bosch & E. H. Bandlien IlJ75 A proposed nomenclature for the main structural features in the Norwegian North Sea. In: K. G. Finstad & R. C. ): Jurassic northern North Sea Symposium (Stavanger) - Norwegian Petroleum Society: 12 pp. Ziegler, P. A. 1981 Evolution of sedimentary basins in north-west Europe. In: L. V. Illing & D. C. ): Petroleum geology of the continental shelf of north-west Europe - Inst.
In Late Triassic - Jurassic , th e eastern fault and possibly also the western fault have been reactivated an d delimit the distribution of the Late Jurassic sediments. The Graben is also in this area a Triassic halfgraben . There is only minor fault activity observed after Jurassic time. Section 3 - A cross-section in the central part of th e area. where the Graben intersects the East North Sea High and the IIolmsland Block (sensu stricto). The western fault here also has a considerable throw.
Petroleum Geology of the Southeastern North Sea and the Adjacent Onshore Areas: (The Hague, 1982) by T. P. Harding (auth.), J. P. H. Kaasschieter, T. J. A. Reijers (eds.)
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