Fig. 7: Radial faults around the central uplift at the BCU level allow reconstruction of the impact trajectory. | Nature Communications

Fig. 7: Radial faults around the central uplift at the BCU level allow reconstruction of the impact trajectory.

From: Multiple lines of evidence for a hypervelocity impact origin for the Silverpit Crater

Fig. 7

True vertical depth subsea (TVDSS) structure maps (a) and dip attribute maps (b) of the Base Cretaceous unconformity, generated from both the Greater NEP 3D and PGS SNS 3D MegaMerge seismic volumes. The yellow arrow shows the axis of bilateral symmetry representing the impact trajectory.

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