Caldera collapse and tectonics along the Main Ethiopian Rift: reviewing possible relationships

The Main Ethiopian Rift (MER) represents an area where volcanism and tectonics interact to create closely linked volcano-tectonic features. This linkage is paramount in the axial portion of the rift, where magmatic segments localize several large peralkaline eruptive centres. Many of them evolved in...

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Veröffentlicht in:Academie des Sciences. Comptes Rendus. Geoscience 2021-01, Vol.353 (S2), p.91-109
Hauptverfasser: Maestrelli, Daniele, Corti, Giacomo, Bonini, Marco, Montanari, Domenico, Sani, Federico
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Sprache:eng
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Zusammenfassung:The Main Ethiopian Rift (MER) represents an area where volcanism and tectonics interact to create closely linked volcano-tectonic features. This linkage is paramount in the axial portion of the rift, where magmatic segments localize several large peralkaline eruptive centres. Many of them evolved into caldera collapse (the best preserved of which are younger than
ISSN:1631-0713
1778-7025
1778-7025
DOI:10.5802/crgeos.63