Extremely voluminous magmatic systems known as large igneous provinces (LIPs)
punctuate Earth's history, and the gases they release plausibly link large-scale geodynamic …

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 …

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

The magmatic components of continental Large Igneous Provinces (LIPs) include flood
basalts and their plumbing system of giant mafic dyke swarms (radiating, linear, and the …

Decades of studies at divergent plate margins have revealed networks of magmatic sills at
the crust-mantle boundary. However, a lack of direct observations of deep magma motion …

Application of 3D seismic reflection data to igneous systems in sedimentary basins has led
to a revolution in the understanding of mafic sill complexes. However, there is considerable …

The movement of magma in sedimentary basins often occurs through an extensive and
interconnected complex of sills. Field‐, modelling‐, and seismic reflection‐based studies …

Even though dykes are the main upward magma pathways through the Earth's crust, the last
two decades of research showed that significant parts of volcano plumbing systems consist …

In this study, we identify a giant circumferential mafic dyke swarm associated with the 135–
75 Ma High Arctic Large Igneous Province (HALIP). Previously, a HALIP giant radiating …

Field and seismic observations show that numerous sills exhibit lobate morphologies. Each
lobe corresponds to a distinct igneous segment exhibiting a finger-like shape, the long axis …