Abstract
Summary There is great uncertainty connected to the definition and recognition of the Skagerrak and Smith Bank formations in the Central North Sea. However, the observations from well logs integrated with seismic lines described below, suggest that these two formations can be time equivalent. In seismic lines, the Triassic succession can be divided into two seismic units based on the seismic character: Seismic Unit 1 is characterized by chaotic and discontinuous reflectors, and it is located at the base of the salt mini-basins. Seismic Unit 2 is characterized by continuous, parallel reflectors in the upper part of the mini-basins.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
