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 …

Geological and geophysical data from continental volcanic centers and giant radial swarms,
and from oceanic shield volcanoes and rift zones, indicate that dikes propagate laterally for …

Tectonic earthquake swarms (TES) often coincide with aseismic slip and sometimes
precede damaging earthquakes. In spite of recent progress in understanding the …

Abstract The Miocene Columbia River Basalt Group (CRBG) is the youngest and best
studied continental flood basalt province on Earth. The 210,000 km3 of basaltic lava flows in …

Singhbhum Craton (SC) hosted eight different dyke swarm events, which are collectively
known as the Newer Dolerite Dykes. These have been correlated with different cratons and …

Clusters of small-volume volcanoes that individually may be defined as monogenetic, but
have interlinked and interconnected plumbing systems, are used to be categorized as …

Volcanic tremor and long period (LP) events are typical seismic signals recorded on active
volcanoes and are characterized by different durations, longer than minutes and a few …

Mantle rocks at oceanic spreading centers reveal dramatic rheological changes from
partially molten to solid‐state ductile to brittle deformation with progressive cooling. Using …

Natural and engineered swarms of hydraulic fractures have been shown to exhibit emergent
geometric characteristics. Fracture spacing, in particular, is often observed to be remarkably …

It is well known that many brittle failure processes follow self-similar scaling relationships.
Both tectonic earthquakes and fractures created during laboratory experiments have source …