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Submarine pingoes: Indicators of shallow gas hydrates in a pockmark at Nyegga, N...
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Comparison and implications from strikingly different authigenic carbonates in a...
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Seep carbonate formation controlled by hydrothermal vent complexes: a case study...
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Climatic and societal impacts of a volcanic double event at the dawn of the Midd...
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Climatic and societal impacts of a volcanic double event at the dawn of the Midd...
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Sill emplacement and contact metamorphism in a siliciclastic reservoir on Svalba...
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Marine diagenesis of tephra aided the Palaeocene-Eocene Thermal Maximum terminat...
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Release of mercury during contact metamorphism of shale: Implications for unders...
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Thermogenic methane release as a cause for the long duration of the PETM
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Temperature changes across the Paleocene-Eocene Thermal Maximum – a new high-res...
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Thermogenic methane release as a cause for the long duration of the PETM
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Thermogenic methane release as a cause for the long duration of the PETM
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Tracing North Atlantic volcanism and seaway connectivity across the Paleocene–Eo...
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Thinking about LIPs: A brief history of ideas in Large igneous province research
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Sill and lava geochemistry of the mid-Norway and NE Greenland conjugate margins
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Thermogenic methane release as a cause for the long duration of the PETM.
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(Table 1) Summary of sampling points described and main petrographic, morphologi...
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U–Pb geochronology of Cretaceous magmatism on Svalbard and Franz Josef Land, Bar...
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(Table 1) Summary of sampling points described and main petrographic, morphologi...
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Rapid and sustained environmental responses to global warming: the Paleocene–Eoc...
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