Magma from the mantle meets the ocean at seafloor spreading centres. At young rifts, basalt sills may heat overlying sediments and induce natural carbon release; basalt flows elsewhere may offer secure reservoirs for sequestration of anthropogenic carbon.
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References
Macdonald, K. C. Annu. Rev. Earth Plan. Sci. 10, 155–190 (1982).
Lizarralde, D., Soule, S. A., Seewald, J. S. & Proskurowski, G. Nature Geosci. 4, 50–54 (2011).
Jamtveit, B., Svense, H., Podladchikov, Y. Y. & Planke, S. in Physical Geology of High-Level Magmatic Systems Vol. 234 (eds Breikreuz, C. & Petford, N) 233–241 (Geological Society of London, special publications, 2004).
Svensen, H. et al. Nature 429, 542–545 (2004).
Einsele, G. Geology 13, 249–252 (1985).
Einsele, G. et al. Nature 283, 441–445 (1980).
Whitcar, M. J. Chem. Geol. 161, 291–314 (1999).
Le Quere, C. et al. Nature Geosci. 2, 831–836 (2009).
Schrag, D. Science 315, 812–813 (2007).
Matter, J. M. & Kelemen, P. B. Nature Geosci. 2, 837–841 (2009).
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Goldberg, D. Carbon below the sea floor. Nature Geosci 4, 11–12 (2011). https://doi.org/10.1038/ngeo1019
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DOI: https://doi.org/10.1038/ngeo1019
