Earthquake swarms are ubiquitous in volcanic systems, being manifestations of underlying
nontectonic processes such as magma intrusions or volatile fluid transport. The Long Valley …

Mantle plumes are one of the most influential first-order tectonic systems on Earth, playing a
prominent role in controlling local magmatic activity and seismicity. Recent studies have …

Abstract The Taupō Volcanic Zone (TVZ) is the southern extent of the Tonga‐Kermadec
volcanic arc and encompasses the Taupō Rift, with the two structures accommodating …

In the North Volcanic Zone of Iceland, we studied with the greatest possible detail the
complete structural architecture and kinematics of the whole Theistareykir Fissure Swarm …

In the Coast Mountains of western British Columbia, an anomalous seismicity concentration
exists near the intersection of the Coast Shear Zone, a major northwest–southeast trending …

In the present work, we have obtained a detailed, complete view of surface deformation at a
volcano-tectonic structure belonging to the Krafla Fissure Swarm (NE Iceland), through the …

In the Northern Volcanic Zone of Iceland, the geometry, kinematics and offset amount of the
structures that form the active Krafla Rift were studied. This rift is composed of a central …

Abstract THE PRECURSORY ACCELERATION OF DEFORMATION is widely validated as a
method for predicting the failure time. Damage evolution inside rocks generally results in …

We present high-quality focal mechanisms and stress inversions based on a refined
earthquake location catalog for the Yellowstone Plateau. The relocation process is based on …

Fractures with transcurrent and oblique components of motion, parallel and coeval to rift
zones, which developed at the surface and in the upper ten kilometers of the crust, have …