Two papers have been published recently on the Cleaver Bank High highlighting the tectonic complexity of this area and its relevance for studying this area for its geothermal energy potential:
Oxford Earth Sciences on the Mull Dyke Swarm (https://lnkd.in/erY-57rR)
Cardiff University on geothermal potential: https://lnkd.in/evmY-85g
Legacy seismic data can be used to help interpret the complex tectonic history. On the left is the Top Chalk Horizon two-way-time. The expression of a dyke at the paleo-seafloor can be seen as a WNW lineament at 'B'. Its corresponding relief map on the right brings out much more clearly a system of faults hardly visible on the regular map and allows to investigate possible interaction with the underlying salt and fault reactivation.
Open Seismic Data: https://lnkd.in/eN7uay_r