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...
Gespeichert in:
Veröffentlicht in: | Academie des Sciences. Comptes Rendus. Geoscience 2021-01, Vol.353 (S2), p.91-109 |
---|---|
Hauptverfasser: | , , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
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 |