Partial desiccation of the Mediterranean Sea may have boosted magmatism during the Messinian epoch.
References
Gudmundsson, A. J. Geophys. Res. 91, 12711–12721 (1986).
Jull, M. & McKenzie, D. J. Geophys. Res. 101, 21815–21828 (1996).
Huybers, P. J. & Langmuir, C. H. Earth Planet. Sci. Lett. 286, 479–491 (2009).
Lund, D. C. & Asimow, P. D. Geochem. Geophys. Geosyst. 12, 12009 (2011).
Crowley, J. W., Katz, R. F., Huybers, P., Langmuir, C. H. & Park, S. H. Science 347, 1237–1240 (2015).
Olive, J.-A. et al. Science 350, 310–313 (2015).
Sternai, P. et al. Nat. Geosci. 10, 783–787 (2017).
Hsü, K. J., Ryan, W. B. & Cita, M. Nature 242, 240–244 (1973).
Faccena, C. & Becker, T. Nature 465, 602–605 (2010).
Keller, T., May, D. A. & Kaus, B. J. P. Geophys. J. Int. 195, 1406–1442 (2013).
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Olive, JA. When less water means more fire. Nature Geosci 10, 718–719 (2017). https://doi.org/10.1038/ngeo3040
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DOI: https://doi.org/10.1038/ngeo3040
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