We have mapped and constrained the timing of tectonically deformed uplifted Late
Quaternary palaeoshorelines in the Messina Strait, southern Italy, an area above a …

Abstract Knowledge of earthquake source faults is crucial for the calculation of robust
Coulomb stress models. However, source faults are often poorly constrained, especially for …

Paleoseismic evidence from the late‐interseismic Alpine Fault suggests key section
boundaries conditionally inhibit rupture. We utilize a year of data from a two‐part …

Intermediate-depth seismicity is common in subducting slabs and the seismicity rate shows
some statistically significant yet enigmatic global positive correlation with the maximal throw …

The condition of stress and recent seismicity in the seismic-prone area can be statistically
analyzed with the Gutenberg-Richter relation (=-). We apply this relation to the hypocenter …

During earthquakes, fault rupture can involve multiple segments in synchronous or cascade
mechanisms, leading to an increasing magnitude of the mainshock or rate of aftershocks …

Surface faulting earthquakes are known to cluster in time from historical and palaeoseismic
studies, but the mechanism (s) responsible for clustering, such as fault interaction, strain …

We determine optimal on‐fault earthquake spatial distributions using a combinatorial
method that minimizes the long‐term cumulative stress resolved on the fault. An integer …

We model Coulomb stress transfer (CST) due to 30 strong earthquakes occurring on normal
faults since 1509 CE in Calabria, Italy, including the influence of interseismic loading, and …

Co-seismic failure can occur on newly formed or on inherited structures. However,
understanding their surface pattern is challenging when pre-existing structural anisotropies …