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The Coupled Magmatic and Hydrothermal Systems of the Restless Aluto Caldera, Ethiopia

Published version
Peer-reviewed

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Authors

Wilks, M. 
Rawlinson, N. 
Kendall, J.-M. 
Nowacki, A. 
Biggs, J. 

Abstract

Seismicity can be used to better understand interactions between magma bodies, hydrothermal systems and their host rocks—key factors influencing volcanic unrest. Here, we use earthquake data to image, for the first time, the seismic velocity structure beneath Aluto, a deforming volcano in the Main Ethiopian Rift. Traveltime tomography is used to jointly relocate seismicity and image 3D P- and S-wave velocity structures and the ratio between them (V P/V S). At depths of 4–9 km, the seismicity maps the top of a large low velocity zone with high V P/V S, which we interpret as a more ductile and melt-bearing region. A shallow (<3 km) hydrothermal system exhibits low seismic velocities and very low V P/V S (∼1.40), consistent with the presence of gases exsolved from a deeper melt-rich mush body. The Artu Jawe fault and fracture system provides the migration pathway that connects the deeper mush body with the shallow hydrothermal system. Together, these observations demonstrate that the interaction between magmatic and hydrothermal systems, driven by the exchange of fluids, is responsible for the restless behavior of Aluto.

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Keywords

Earth Science, tomography, volcano seismicity, magmatic systems, hydrothermal, systems, seismic imaging, restless volcano

Journal Title

Frontiers in Earth Science

Conference Name

Journal ISSN

2296-6463

Volume Title

8

Publisher

Frontiers Media S.A.