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      Mid-Norwegian Margin Magmatism and Paleoclimate Implications 

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          Magmatism at rift zones: The generation of volcanic continental margins and flood basalts

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            Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene

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              Large igneous provinces and mass extinctions

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                April 06 2023
                10.14379/iodp.proc.396.101.2023
                826a0b29-51a3-43b6-a65f-b899557d4e52
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