Stress barriers controlling lateral migration of magma revealed by seismic tomography


Understanding how monogenetic volcanic systems work requires full comprehension of the local and regional stresses that govern magma migration inside them and why/how they seem to change from one eruption to another. During the 2011-2012 El Hierro eruption (Canary Islands) the characteristics of unrest, including a continuous change in the location of… (More)
DOI: 10.1038/srep40757


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