Ductility and Compressibility Accommodate High Magma Flux Beneath a Silicic Continental Rift Caldera: Insights From Corbetti Caldera (Ethiopia)

Large silicic magma reservoirs preferentially form in the upper crust of extensional continental environments. However, our quantitative understanding of the link between mantle magmatism, silicic reservoirs, and surface deformation during rifting is very limited. Here, we focus on Corbetti, a peral...

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Bibliographic Details
Published in:Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2020-04, Vol.21 (4), p.n/a
Main Authors: Gottsmann, J., Biggs, J., Lloyd, R., Biranhu, Y., Lewi, E.
Format: Article
Language:English
Subjects:
caldera
Calderas
Compressibility
Deformation
Ductility
Gravity
gravity changes
Lava
Mafic magma
Magma
Magma chambers
Mass flux
Population density
Reservoirs
Rifting
Upper mantle
volcano geodesy
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Summary:Large silicic magma reservoirs preferentially form in the upper crust of extensional continental environments. However, our quantitative understanding of the link between mantle magmatism, silicic reservoirs, and surface deformation during rifting is very limited. Here, we focus on Corbetti, a peralkaline caldera in the densely populated Main Ethiopian Rift, which lies above a focused zone of upper mantle partial melt and has been steadily uplifting at a maximum rate of 6.6±1.2 cm yr−1 for more than 10 yr. Numerical modeling shows that a maximum concomitant residual gravity increase of 9±3 μGal yr−1 by the intrusion of mafic magma at ∼7 km depth into a compressible and inelastic crystal mush best explains the observed deformation and gravity changes. The derived magma mass flux of ∼1011 kg yr−1 is anomalously high and at least 1 order of magnitude greater than the mean long‐term mass eruption rate. This study demonstrates that periodic and high‐rate magmatic rejuvenation of upper‐crustal mush is a significant and rapid contributor to mature continental rifting. Key Points Corbetti caldera is undergoing unrest since 2009 with a maximum uplift rate of 6.6 cm yr−1 Net mass addition at 6–8 km below the surface by anomalously high magma flux (1.1 to 2.0×1011 kg yr−1) accommodated into compressible and inelastic upper‐crustal crystal mush Deformation of thermomechanically heterogenous host rock dominates mass redistribution and associated gravity changes
ISSN:1525-2027
1525-2027
DOI:10.1029/2020GC008952