The K-alkaline, Quaternary Roman Magmatic Province (RMP) includes several active...
The eruptive style of mafic volcanoes is critically influenced by magma rheology,...
Crystallisation kinetics play a fundamental role in controlling conduit dynamics...
Paroxysmal mafic activity is a relevant source of hazard at many active volcanoes....
Understanding the rheological evolution of solidifying magma during its migration...
Stromboli is a unique open-conduit mafic volcano known for persistent Strombolian...
The 472 CE sub-Plinian eruption of Somma-Vesuvius represents a critical reference...
Small- to moderate-volume eruptions at caldera systems often involve complex and...
Throughout Earth’s history, eruptions from volcanic fissures have been responsible...
Reconstructing the eruptive history of Antarctic volcanoes is often challenging due...
Active insular volcanoes are generally characterized by their rapid morphological...
Sill emplacement is fundamental to the development of volcanic plumbing systems and...