Towards a process-based understanding of rifted continental margins
Author:
Publisher
Springer Science and Business Media LLC
Subject
Nature and Landscape Conservation,Atmospheric Science,Earth-Surface Processes,Pollution
Link
https://www.nature.com/articles/s43017-022-00380-y.pdf
Reference223 articles.
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2. Planke, S., Berndt, C. & Alvarez Zarikian, C. A. Expedition 396 scientific prospectus: mid-Norwegian continental margin magmatism. Sci. Prospectuses Int. Ocean. Discov. Program https://doi.org/10.14379/iodp.sp.396.2021 (2021).
3. Brune, S., Williams, S. E. & Müller, R. D. Potential links between continental rifting, CO2 degassing and climate change through time. Nat. Geosci. 10, 941–946 (2017).
4. Svensen, H. et al. Release of methane from a volcanic basin as a mechanism for initial Eocene global warming. Nature 429, 542–545 (2004).
5. Pérez-Gussinyé, M. et al. Serpentinization and magmatism during extension at non-volcanic margins: the effect of initial lithospheric structure. Geol. Soc. Spec. Publ. https://doi.org/10.1144/gsl.Sp.2001.187.01.27 (2001).
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