Understanding the initiation and arrest of earthquakes is one of the
long-standing challenges of seismology. Here we report on direct
observations of borehole displacement by a meter-sized shear rupture
induced by pressurization of metamorphic rock at 1.5 km depth. We
observed the acceleration of sliding, followed by fast co-seismic slip
and transient afterslip. Total displacements were about 7, 5.5 and 9.5
micrometers, respectively for the observed pre-slip, co-seismic slip and
afterslip. The observed pre-slip lasted about 0.4 seconds. Co-seismic
slip was recorded by the 1 kHz displacement recording and a 12-component
array of 3-C accelerometers sampled at 100 kHz. The observed afterslip
is consistent with analytical models of arrest in a
velocity-strengthening region and subsequent stress relaxation.

The observed slip vector agrees with the activation of a bedding plane
within the phyllite, which is corroborated by relocated seismic events
that were observed during the later stages of the injection experiment.