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Magma storage conditions beneath a peralkaline caldera in the Main Ethiopian Rift

Title: Magma storage conditions beneath a peralkaline caldera in the Main Ethiopian Rift
Authors: Colby, David, J; Pyle, David, M; Fontijn, Karen; Mather, Tamsin, A; Nomade, Sebastien; Melaku, Abate, A; Mengesha, Million, A; Yirgu, Gezahegn
Contributors: Department of Earth Sciences Oxford; University of Oxford; Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE); Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)); Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA); Paléocéanographie (PALEOCEAN); Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Source: ISSN: 0377-0273 ; Journal of Volcanology and Geothermal Research ; https://hal.science/hal-04678917 ; Journal of Volcanology and Geothermal Research, 2024, pp.108165. ⟨10.1016/j.jvolgeores.2024.108165⟩.
Publisher Information: CCSD; Elsevier
Publication Year: 2024
Collection: Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ
Subject Terms: Peralkaline Geochemistry Petrology RhyoliteMELTS Alkali Basalt; Peralkaline; Geochemistry; Petrology; RhyoliteMELTS; Alkali Basalt; [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces; environment
Description: International audience ; The numerous volcanic centres in the Main Ethiopian Rift (MER) present significant but poorly understood hazards to local populations. The MER is also an important site to gain insights into tectonic processes as it captures the transition from continental rifting (to the south) to incipient seafloor spreading (to the north). Peralkaline magmas account for around 90% of the volcanic products found in the MER. Determining the conditions under which these magmas evolve is critical to understanding rift-related volcanism and its associated hazards. Corbetti Caldera has an extensive record of large-scale, predominantly aphyric, peralkaline rhyolite eruptions. However, little is known about the mafic magmas from which these highly differentiated melts have evolved. Here we present data from the only basaltic deposit found within the caldera, coupled with whole rock, glass and mineral analysis of the peralkaline products, to investigate magma storage conditions at Corbetti. We demonstrate that magma mixing played a role in the evolution of the basaltic magmas and use RhyoliteMELTS modelling to show Corbetti's peralkaline magmas likely evolved at pressures between 100 and 250 MPa, from a magma with an initial water content of 0.5 -1 wt.%, at or below the QFM buffer. Mineral hygrometry on the sparse crystal populations corroborates the RhyoliteMELTS J o u r n a l P r e -p r o o f Journal Pre-proof modelling, suggesting that the basaltic magma had 0.1-1.2 ± 0.32 wt.% H2O, and the peralkaline magmas an average of ~5.5 ± 1.25 wt.% H2O. These results also match melt inclusion data for Corbetti and other peralkaline systems. We also provide new 40 Ar/ 39 Ar sanidine ages for two eruptions, a pre-caldera rhyolitic lava flow (206.7 ± 0.9 ka) and a postcaldera peralkaline ignimbrite (160 ± 0.8 ka). These results add to our understanding of the history of Corbetti and the storage conditions of peralkaline magmas within a continental rift setting and highlight the hydrous nature of Corbetti's magmas and ...
Document Type: article in journal/newspaper
Language: English
DOI: 10.1016/j.jvolgeores.2024.108165
Availability: https://hal.science/hal-04678917; https://hal.science/hal-04678917v1/document; https://hal.science/hal-04678917v1/file/1-s2.0-S0377027324001574-main.pdf; https://doi.org/10.1016/j.jvolgeores.2024.108165
Rights: https://about.hal.science/hal-authorisation-v1/ ; info:eu-repo/semantics/OpenAccess
Accession Number: edsbas.6CA0C65D
Database: BASE