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 …

We review the numerous experimental studies dedicated to unravelling the physics and
dynamics of various parts of a volcanic plumbing system. Section 1 lists the model materials …

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

A voluminous magmatic complex was emplaced in the Vøring and Møre basins during
Paleocene/Eocene continental rifting and break-up in the NE Atlantic. This intrusive event …

The climate change in the Toarcian (Early Jurassic) was characterized by a major
perturbation of the global carbon cycle. The event lasted for approximately 200,000 years …

A series of experiments are described where dyed water (a magma analogue) was intruded
into solid gelatine (a crustal analogue) to investigate the formation of sills. We considered a …

Many seismic and magnetotelluric experiments within Tibet provide proxies for lithospheric
temperature and lithology, and hence rheology. Most data have been collected between c …

Magmatic sheet intrusions contribute significantly to the upper crustal magma transport
network. The emplacement mechanism of the magmatic sheets controls the final geometry of …

Forced folds formed at the seabed immediately overlying shallow (< 1km) saucer-shaped
sills along the NE Atlantic Margin during the early Paleogene. Examples of this sill-fold …

Magmatic intrusions and fluidized injected sands represent the two main types of sheet
intrusions in the Earth's crust. In this paper we show that both intrusion types often display a …