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The evolution of magma during continental rifting : new constraints from the isotopic and trace element signatures of silicic magmas from Ethiopian volcanoes

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Figure

Table 1. Summary of the geological setting, eruptive history and age constraints for the six
Table 2. New oxygen isotope data for Ethiopian volcanic systems.
Table 3. Best-fit magma storage conditions for Aluto and Dabbahu constrained via Rhyolite-
Table 4. Erupted and cumulate volume estimates for the volcanic systems considered in this

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