Articles | Volume 26
https://doi.org/10.5194/sd-26-69-2019
https://doi.org/10.5194/sd-26-69-2019
Workshop white paper
 | 
02 Dec 2019
Workshop white paper |  | 02 Dec 2019

Northeast Atlantic breakup volcanism and consequences for Paleogene climate change – MagellanPlus Workshop report

Christian Berndt, Sverre Planke, Damon Teagle, Ritske Huismans, Trond Torsvik, Joost Frieling, Morgan T. Jones, Dougal A. Jerram, Christian Tegner, Jan Inge Faleide, Helen Coxall, and Wei-Li Hong

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Cited articles

Aarnes, I., Svensen, H., Connolly, J. A., and Podladchikov, Y. Y.: How contact metamorphism can trigger global climate changes: Modeling gas generation around igneous sills in sedimentary basins, Geochem. Cosmochem. Ac., 74, 7179–7195, 2010. 
Aarnes, I., Svensen, H., Polteau, S., and Planke, S.: Contact metamorphic devolatilization of shales in the Karoo Basin, South Africa, and the effects of multiple sill intrusions, Chem. Geol., 281, 181–194, 2011. 
Aarnes, I., Planke, S., Trulsvik, M., and Svensen, H.: Contact metamorphism and thermogenic gas generation in the Vøring and Møre basins, offshore Norway, during the Paleocene–Eocene thermal maximum, J. Geol. Soc., 172, 588–598, 2015. 
Abdelmalak, M. M., Planke, S., Faleide, J. I., Jerram, D. A., Zastrozhnov, D., Eide, S., and Myklebust, R.: The development of volcanic sequences at rifted margins: New insights from the structure and morphology of the Vøring Escarpment, mid-Norwegian Margin, J. Geophys. Res., 121, 5212–5236, 2016. 
Abdelmalak, M. M., Planke, S., Polteau, S., Hartz, E. H., Faleide, J. I., Tegner, C., Jerram, D. A., Millett, J. M., and Myklebust, R.: Breakup volcanism and plate tectonics in the NW Atlantic, Tectonophysics, 760, 267–296, 2019. 
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Short summary
The northeast Atlantic encompasses archetypal examples of volcanic rifted margins. Twenty-five years after the last ODP leg on these volcanic margins, the reasons for excess melting are still disputed with at least three competing hypotheses being discussed. We are proposing a new drilling campaign that will constrain the timing, rates of volcanism, and vertical movements of rifted margins.