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  1. No Access

    Chapter

    Geophysics and Remote Sensing

    Igneous sheet intrusions such as sills, dikes, and laccoliths are abundant in volcanic basins. Mafic intrusions are characterized by high in the range from 5.0 to 7.0 km/s. Velocity aureoles with a thickness ...

    Sverre Planke, Henrik Svensen in Physical Geology of Shallow Magmatic Syste… (2018)

  2. Article

    Open Access

    Climatic and societal impacts of a volcanic double event at the dawn of the Middle Ages

    Volcanic activity in and around the year 536 CE led to severe cold and famine, and has been speculatively linked to large-scale societal crises around the globe. Using a coupled aerosol-climate model, with eru...

    Matthew Toohey, Kirstin Krüger, Michael Sigl, Frode Stordal in Climatic Change (2016)

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    Article

    A petrologic, geochemical and Sr–Nd isotopic study on contact metamorphism and degassing of Devonian evaporites in the Norilsk aureoles, Siberia

    Devonian evaporites and associated sedimentary rocks in the Norilsk region were contact metamorphosed during emplacement of mafic sills that form part of the end-Permian (~252 Ma) Siberian Traps. We present mi...

    Kwan-Nang Pang, Nicholas Arndt, Henrik Svensen in Contributions to Mineralogy and Petrology (2013)

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    Article

    Bubbles from the deep

    A study suggests that hydrocarbons released from sedimentary basins formed part of a climatic feedback mechanism that exacerbated global warming during the Eocene epoch.

    Henrik Svensen in Nature (2012)

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    Article

    Release of methane from a volcanic basin as a mechanism for initial Eocene global warming

    A 200,000-yr interval of extreme global warming marked the start of the Eocene epoch about 55 million years ago. Negative carbon- and oxygen-isotope excursions in marine and terrestrial sediments show that thi...

    Henrik Svensen, Sverre Planke, Anders Malthe-Sørenssen, Bjørn Jamtveit in Nature (2004)

  6. No Access

    Article

    Seep carbonate formation controlled by hydrothermal vent complexes: a case study from the Vøring Basin, the Norwegian Sea

    Several hundred hydrothermal vent complexes were formed in the Vøring Basin as a consequence of magmatic sill emplacement in the late Palaeocene. The 6607/12-1 exploration well was drilled through a 220-m-thic...

    Henrik Svensen, Sverre Planke, Bjørn Jamtveit, Tom Pedersen in Geo-Marine Letters (2003)