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2. Evolution of a magma-driven earthquake swarm and triggering of the nearby Oldoinyo Lengai eruption, as resolved by InSAR, ground observations and elastic modeling, East African Rift, 2007;['Baer, G.', 'Hamiel, Y.', 'Shamir, G.', 'Nof, R.'];Earth Planet. Sci. Lett.,2008
3. Trace element partitioning between wollastonite and alkaline silicate magmas;['Baudouin, C.', 'France, L.'];Chem. Geol.,2019
4. Trace element partitioning between clinopyroxene and alkaline magmas;['Baudouin, C.', 'France, L.', 'Boulanger, M.', 'Dalou, C.', 'Devidal, J. L.'];Contrib. Mineral. Petrol.,2020
5. Carbonatite and highly peralkaline nephelinite melts from Oldoinyo Lengai volcano, Tanzania: The role of natrite-normative fluid degassing;['Berkesi, M.', 'Bali, E.', 'Bodnar, R. J.', 'Szabó, Á.', 'Guzmics, T.'];Gondwana Res.,2020