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Beryl湾位于北海维京地堑的最南端,有三组断层,走向分别为北东向、北西—南东向和北东—南西向。本文利用73口井的高分辨率沉降分析,结合部分区域地震,来阐述中—晚侏罗世的沉降模式。已经完成的高分辨率(每个点间隔仅1～2Ma)沉降分析可以用来研究不同走向断层的时间演化,以及
Beryl Bay is located at the southernmost tip of the Viking Graben in the North Sea. It has three groups of faults that run north-east, north west-south-east and north-east-south west. In this paper, 73 wells in high resolution settlement analysis, combined with some regional earthquakes to explain the mid-late Jurassic settlement mode. Completed high-resolution (only 1 to 2Ma intervals) of subsidence analysis can be used to study the temporal evolution of different strike-faults and