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 …

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 deformation associated with several small, brittle faults was investigated on both
microscopic and macroscopic scales. While the dominant macroscopic structures are …

Sandstone intrusions are found in all sedimentary environments but have been reported
most commonly from deep-water settings. They also appear to be more frequently …

Late Miocene sills and dikes in the Paiute Ridge area of southern Nevada were emplaced in
an extensional setting beneath a small volume, alkali basaltic volcanic center. Dikes (400 …

The Aeolian volcanoes are located between the Southern Tyrrhenian Sea back arc and the
Calabrian Arc forearc region. Structural, geochemical and seismological data indicate that …

The opening of a fracture is dependent on the fluid pressure and the local stress regime
around the fracture. For a fracture to open, the fluid pressure must exceed the normal stress …

Fault stability evaluation is crucial for ensuring safety of underground gas storage (UGS)
reconstructed from depleted oil and gas reservoirs. To make assessment result more …

A two‐dimensional numerical model for coupled elastic deformation and fluid flow has been
developed to examine reinitiation or termination of a vertical fluid‐driven fracture in bedded …

The dykes of the Mull swarm, part of the British Tertiary Igneous Province, have been
examined in a series of well exposed coastal sections. Traverses through the dyke swarm …