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                <full_title>Geological Society, London, Special Publications</full_title>
                <abbrev_title>SP</abbrev_title>
                <issn media_type="print">0305-8719</issn>
                <issn media_type="electronic">2041-4927</issn>
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                  <day>28</day>
                  <year>2022</year>
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                  <title>Cross-basin Mo and U analysis of the Upper Mississippian Bowland Shale, UK</title>
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                    <given_name>Jack</given_name>
                    <surname>Walker</surname>
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                      <institution>
                        <institution_name>Edge Hill University</institution_name>
                        <institution_place>Ormskirk, UK</institution_place>
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                    <given_name>Joseph F.</given_name>
                    <surname>Emmings</surname>
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                        <institution_name>CGG, Tyn Y Coed, Llanrhos, Llandudno LL30 1SA, UK</institution_name>
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                  <person_name contributor_role="author" sequence="additional">
                    <given_name>Sanem</given_name>
                    <surname>Acikalin</surname>
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                      <institution>
                        <institution_name>School of Natural and Environmental Sciences, Newcastle University</institution_name>
                        <institution_place>Newcastle upon Tyne, UK</institution_place>
                      </institution>
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                    <given_name>Shannon</given_name>
                    <surname>Flynn</surname>
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                      <institution>
                        <institution_name>School of Natural and Environmental Sciences, Newcastle University</institution_name>
                        <institution_place>Newcastle upon Tyne, UK</institution_place>
                      </institution>
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                  <person_name contributor_role="author" sequence="additional">
                    <given_name>Cees</given_name>
                    <surname>van der Land</surname>
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                      <institution>
                        <institution_name>School of Natural and Environmental Sciences, Newcastle University</institution_name>
                        <institution_place>Newcastle upon Tyne, UK</institution_place>
                      </institution>
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                    <given_name>Martin</given_name>
                    <surname>Jones</surname>
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                      <institution>
                        <institution_name>School of Natural and Environmental Sciences, Newcastle University</institution_name>
                        <institution_place>Newcastle upon Tyne, UK</institution_place>
                      </institution>
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                  </person_name>
                  <person_name contributor_role="author" sequence="additional">
                    <given_name>Christopher H.</given_name>
                    <surname>Vane</surname>
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                      <institution>
                        <institution_name>British Geological Survey</institution_name>
                        <institution_place>Keyworth, UK</institution_place>
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                  <person_name contributor_role="author" sequence="additional">
                    <given_name>Jan A. I.</given_name>
                    <surname>Hennissen</surname>
                    <affiliations>
                      <institution>
                        <institution_name>British Geological Survey</institution_name>
                        <institution_place>Keyworth, UK</institution_place>
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                  <person_name contributor_role="author" sequence="additional">
                    <given_name>Ed</given_name>
                    <surname>Hough</surname>
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                        <institution_name>British Geological Survey</institution_name>
                        <institution_place>Keyworth, UK</institution_place>
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                  <person_name contributor_role="author" sequence="additional">
                    <given_name>Thomas</given_name>
                    <surname>Wagner</surname>
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                      <institution>
                        <institution_name>The Lyell Centre, Heriot-Watt University</institution_name>
                        <institution_place>UK</institution_place>
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                  <person_name contributor_role="author" sequence="additional">
                    <given_name>Lucy</given_name>
                    <surname>Craddock</surname>
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                      <institution>
                        <institution_name>Cuadrilla Resources Ltd, Manchester Business Park, 3000 Aviator Way, Wythenshawe, Manchester M22 5TG, UK</institution_name>
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                  <jats:title>Abstract</jats:title>
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                    The Bowland sub-basin is a target for hydrocarbon exploration, but to a large extent it remains unexplored. To determine the economic potential of the Bowland sub-basin, it is important to identify the oceanographic processes involved in the deposition of the Bowland Shale Formation in the Late Mississippian (
                    <jats:italic>c.</jats:italic>
                    330 Ma). Palaeoceanographic processes are known to be a major control on the development of hydrocarbon source rocks. This study investigates core (Preese Hall-1 and Becconsall-1Z) materials from the Upper Bowland Shale, and makes a comparison with previously published data (outcrop Hind Clough), all from the Bowland sub-basin, Lancashire, UK. The sedimentology and geochemistry of this formation were determined via a multi-technique approach including X-ray fluorescence, sedimentology, gamma-ray spectra, X-ray diffraction and Rock-Eval pyrolysis. Key trace metal abundances and enrichment factors were used to assess sediment provenance and to determine the bottom-water redox conditions during the deposition of the Upper Bowland Shale. Our results support interpretations of contemporaneous anoxia developing in bottom waters in at least three sites in the Bowland sub-basin. In a comparison with the Fort Worth Basin (Barnett Shale, USA), the Bowland sub-basin was apparently less restricted and deposited under a much higher mean sediment accumulation rate. Knowledge from this study will improve future resource estimates of the Bowland Shale Formation, and challenge the early assumptions that the Barnett Shale is an analogue of the Bowland Shale.
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                  <last_page>164</last_page>
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