Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur
in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas …

Many continental rifts are subjected to volcanism in tandem with rifting, which has raised a
long-standing debate about whether magmatism is the cause or the consequence of plate …

Plate motion and associated tectonics explain the location of magmatic systems along plate
boundaries [1], however, they cannot give satisfactory explanations of the origin of intra …

Monogenetic basaltic volcanic fields occur worldwide in tectonic environments ranging from
extensional to convergent. Understanding similarities and differences between these fields …

Monogenetic basaltic volcanism is characterised by a complex array of behaviours in the
spatial distribution of magma output and also temporal variability in magma flux and eruptive …

Most of Earth's volcanism occurs at plate boundaries, in association with subduction or
rifting. A few high-volume volcanic fields are observed both at plate boundaries and within …

High-resolution, stratigraphically ordered samples of the Udo tuff cone and lava shield
offshore of Jeju Island, South Korea, show complex geochemical variation in the basaltic …

Petit-spot volcanoes provide a unique opportunity to directly examine the structure and
geochemical composition of the lithospheric and asthenospheric mantle beneath the …

Magma transport through dikes is a major component of the development of monogenetic
volcanic fields. These volcanic fields are characterized by numerous volcanic centers, each …

Interactions between volcanic and tectonic processes affect the distribution, morphology,
and volume of eruptive products in space and time. The Queréndaro area in the eastern …