Magma transport in brittle rock occurs by diking. Understanding the dynamics of diking and
its observable consequences is essential to deciphering magma propagation in volcanic …

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 …

The structure of upper crustal magma plumbing systems controls the distribution of
volcanism and influences tectonic processes. However, delineating the structure and …

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 volcanoes are the most common volcanic landforms on the continents.
They encompass a range of morphologies from small pyroclastic constructs to larger shields …

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

ABSTRACT INTRODUCTION that are commonly, but not exclusively, small in eruptive
volume. Monogenetic volcanic fields commonly consist of large numbers of volcanic clusters …

Magma is transported and stored in the crust mostly through networks of planar structures
(intrusive sheets), ranging from vertical dykes to inclined sheets and horizontal sills, and …

Temporal and spatial changes in volcano morphology and internal architecture can
determine eruption style and location. However, the relationship between the external and …

Felsic and mafic magmas in continental crustal settings are derived by melting of the lower
crust and mantle, respectively. This occurs in subduction zone, collisional, extensional and …