A cascade of magmatic events during the assembly and eruption of a super-sized magma body... Prior to eruption the assembled eruptible magma body was not thermally or compositionally zoned and at temperatures of ~790°C, reflecting rapid cooling from the ~840 °C low-silica rhyolite feedstock magma....
Effects of host-rock fracturing on elastic-deformation source models of volcano deflation... non-elastic deformation) during drainage of a magma body can progressively change the shape and depth of an elastic-deformation source....
The zone 1440 ad eruption of the soufriere of guadeloupe (lesser antilles) : an experimental determination of the pre-eruptive consitions of the andesitic magma body.... This compositional sequence is interpreted to reflect the tapping of a silicic magma body remobilised following the arrival of a mafic magma batch....
Sombrero uplift above the altiplano-puna magma body: evidence of a ballooning mid-crustal diapirThe Altiplano-Puna ultralow-velocity zone in the central Andes, South America, is the largest active magma body in Earth’s continental crust....
