Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

Deep-seated slow slip and tremor (SST), including slow slip events, episodic tremor and
slip, and low-frequency earthquakes, occur downdip of the seismogenic zone of numerous …

The combination of hybrid perovskite and Cu (In, Ga) Se2 (CIGS) has the potential for
realizing high-efficiency thin-film tandem solar cells because of the complementary tunable …

Faults are rarely completely smooth, with topographic undulations coming from the
distribution of asperities along the fault surface. Understanding the effects of fault surface …

Fluid injection can cause extensive earthquake activity, sometimes at unexpectedly large
distances. Appropriately mitigating associated seismic hazards requires a better …

I am grateful to the many people who played a part in the evolution of this book: my
colleagues David McGlynn and Jerald Podair; Princeton University Press editors Eric …

The scaling law for slow earthquakes, which is a linear relationship between seismic
moment and duration, was proposed 15 y ago and initiated a debate on the difference in …

Many large earthquakes are preceded by one or more foreshocks, but it is unclear how
these foreshocks relate to the nucleation process of the mainshock. On the basis of an …

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

Anthropogenic fluid injections at depth induce seismicity which is generally organized as
swarms, clustered in time and space, with moderate magnitudes. Earthquake swarms also …