P736.21
Acknowledgements This project was sponsored by the Royal Society, London, and China Association for Science and Technology. We wish to thank Mobil North Sea Ltd. （Aberdeen） for releasing and providing well log, biostratigraphic and some seismic data. In Edinburgh, we are grateful to John Underhill and Nancye H. Dawers for fruitful discussion and comments, and Gerard White and Chung-Lun Lau for computer support in the Department of Geology and Geophysics.
1 Introduction A series of studies have indicated that there were two extensional phases in the North Sea (Fig. 1). An earlier period (Late Permian-Early Triassic) of rifting occurred widely in these areas, with predominant extension direction of W-E (F?rseth, 1996; F?rseth et al., 1997). In contrast to the widely distributed Permo-Triassic extension, Jurassic extension in the North Sea were generally much more localized into the three main rift arms (Fig. 1): the Viking Graben, Moray…
1 Introduction A series of studies have indicated that there were two extensional phases in the North Sea (Fig. 1). An earlier period (Late Permian-Early Triassic) of rifting occurred widely in these areas, with predominant extension direction of W-E (F?rseth, 1996; F?rseth et al., 1997). In contrast to the widely distributed Permo-Triassic extension, Jurassic extension in the North Sea were generally much more localized into the three main rift arms (Fig. 1): the Viking Graben, Moray…
Jon D. TURNER, Roger A. SCRUTTON.2006. Application of Multi-well Subsidence Analysis of the Beryl Embayment, Viking Graben, Northern North Sea[J]. ACTA GEOLOGICA SINICA(English edition),80(5):693~704
复制
