1. Pre-eruptive storage conditions and magmatic evolution of the Bora-Baricha-Tullu Moye volcanic system, Main Ethiopian Rift
- Author
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Tadesse, AZ, Fontijn, K, Caricchi, L, Bégué, F, Gudbrandsson, S, Smith, VC, Gopon, P, Debaille, V, Laha, P, Terryn, H, Yirgu, G, Ayalew, D, Chemistry, Materials and Chemistry, Electrochemical and Surface Engineering, and Materials and Surface Science & Engineering
- Subjects
Magmatic evolution ,Pre-eruptive storage conditions ,Main Ethiopian Rift ,Geochemistry and Petrology ,Caldera system ,Geology ,Magmatic plumbing system - Abstract
The Main Ethiopian Rift (MER) is a tectonically and magmatically active rift in the northern portion of the East African Rift System. The MER contains around 60 volcanoes with some evidence of activity in the Holocene. Large caldera-hosting silicic volcanoes are dotted along the rift floor, including some with evidence of explosive eruptions every few hundred years. The pre-eruptive storage conditions and magmatic evolution of most MER silicic volcanoes remain poorly understood. The Bora-Baricha-Tullu Moye is a Late Quaternary volcanic system in the MER, characterised by products of both explosive and effusive volcanic eruptions. The petrological and geochemical characteristics of the volcanic products are investigated. The bulk rock compositions vary from basalt to comendite and pantellerite, and the chemical variability can largely be explained by fractional crystallisation processes starting from a transitional basaltic parent magma with minor crustal assimilation and magma mixing. The comendite and pantellerite deposits systematically show variation in glass and mineral compositions along stratigraphy. The combination of thermometry and barometry modelling suggests that the basaltic magma is stored at high temperature (1070-1190 °C) at mid-crustal level (~7-29 km). The peralkaline rhyolite melts are stored at a lower temperature (i.e., 805-900 °C for comendite and 700-765 °C for pantellerite) at shallow crustal levels (~4 km). Stratigraphic evidence in combination with the pre-eruptive storage conditions further elucidates that these shallow peralkaline magmatic reservoirs temporally evolve to cooler storage. , The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)
- Published
- 2023
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