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                  <title>Cross-border subsurface geology in the Atlantic Margin and the Barents Sea: an introduction</title>
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                    <given_name>Domenico</given_name>
                    <surname>Chiarella</surname>
                    <affiliation>Department of Earth Sciences, Queen's Building, Royal Holloway, University of London, Egham, Surrey TW20 0EX, UK</affiliation>
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                    <given_name>Stuart Gordon</given_name>
                    <surname>Archer</surname>
                    <affiliation>Harbour Energy, Rubislaw House, South Anderson Drive, Aberdeen AB15 6FZ, UK</affiliation>
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                    <given_name>John A.</given_name>
                    <surname>Howell</surname>
                    <affiliation>Department of Geology and Geophysics, Meston Building, King's College, Aberdeen AB24 3FX, UK</affiliation>
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                    <given_name>Christopher A.-L.</given_name>
                    <surname>Jackson</surname>
                    <affiliation>Department of Earth and Environmental Sciences, The University of Manchester, Williamson Building, Oxford Road, Manchester M13 9PL, UK</affiliation>
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                    <given_name>Henk</given_name>
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                    <affiliation>North Sea Core, 8 Dubford Terrace, Aberdeen AB23 8GE, UK</affiliation>
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                    <given_name>Stefano</given_name>
                    <surname>Patruno</surname>
                    <affiliation>Department of Engineering, University of Nicosia, 46 Makedonitissas Avenue, CY-2417, PO Box 24005, Nicosia CY-1700, Cyprus</affiliation>
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                    Over the last 50 years, the North Sea and the Atlantic Margin and, more recently the Barents Sea, represented key study areas for academic and professionals interested in the exploration for and production of hydrocarbon from the Earth's subsurface. Nowadays, these areas may play a major role in the so-called ‘energy transition’, with the energy industry now seeking to reduce emissions related to hydrocarbon consumption, and leading the development of carbon capture and storage activities, such as the
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                    ). Consequently, there is an increasing interest in advancing our knowledge regarding the stratigraphy, sedimentology and tectonic development of the North Sea, Atlantic Margin and Barents Sea with a cross-border approach.
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