Solar neon in the Icelandic mantle: new evidence for an undegassed lower mantle: Earth and Planetary

By M. Moreira, K. Breddam, J. Curtice, M. Kurz. 2001

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Observational and theoretical studies of the dynamics of mantle plume–mid‐ocean ridge interaction (2003, unknown): “For example, compared to mid-ocean ridge basalts, OIBs with elevated (more primitive) 3He/4He ratios have lower (more primitive) 21Ne/ 22Ne ratios [Honda et al., 1993; Moreira et al., 2001].”
Water and astrobiology (2007, background): “The highest 20Ne/22Ne ratio measured in OIB from Iceland (13.3; Dixon et al., 2000; Moreira et al., 2001) and from a Devonian carbonatite in an ancient plume setting on the Kola Peninsula, Russia (X13.”
Evidence for multiple magma ocean outgassing and atmospheric loss episodes from mantle noble gases (2013, background): “In contrast, plumes tend to have lower 3 He/ 22 Ne ratios (e.g. Füri et al., 2010; Graham, 2002; Honda and McDougall, 1998; Jackson et al., 2009; Kurz et al., 2009; Moreira et al., 2001; Mukhopadhyay, 2012; Raquin and Moreira, 2009; Yokochi and Marty, 2004).”