We show that near–real-time seismic monitoring of fluid injection allowed control of induced
earthquakes during the stimulation of a 6.1-km-deep geothermal well near Helsinki, Finland …

Uniaxial compression tests with combined acousto-optical monitoring techniques are
conducted on flawed granite specimens, with the aim of investigating the fracture-related …

Dynamic failure in the laboratory is commonly preceded by many foreshocks which
accompany premonitory aseismic slip. Aseismic slip is also thought to govern earthquake …

We examine localization processes of low magnitude seismicity in relation to the occurrence
of large earthquakes using three complementary analyses:(i) estimated production of rock …

We discuss data of three laboratory stick‐slip experiments on Westerly Granite samples
performed at elevated confining pressure and constant displacement rate on rough fracture …

Clustering of earthquake magnitudes is still actively debated, compared to well-established
spatial and temporal clustering. Magnitude clustering is not currently implemented in …

Earthquakes rarely occur in isolation but rather as complex sequences of fore, main and
aftershocks. Assessing the associated seismic hazard requires a holistic view of event …

Accurate knowledge of the spatiotemporal evolution of damage within mechanically loaded
structural elements is of great importance for a wide range of engineering fields. In this …

Aftershock cascades are a characteristic feature of natural seismicity, but underlying
mechanisms remain debated. Here, we experimentally explore the presence or absence of …

The process whereby a brittle fault was activated by mining is not only significant for disaster
prediction, but also for earthquake prediction. Thus, it was necessary to study their activation …