3D crustal-scale fault structure
The 1986 Chalfant Valley EQ Sequence
There were over 20,000 hypocenters assoiated with this earthquake, and they have been double-difference relocated, quite precisely due to the dense seismic network there near the Long Valley Caldera.
I have used this dense array of points to identify the diversity of fault structures that were activated during the protracted EQ.
The results show a unique arrangement of faults and fault intersections. Please see the figures below from preliminary work that is driving new 3D visualization tools for looking at dynamic stress and EQ triggering.
Complex, juvenile fault systems such as this pose significant seismic risk. Some faults become super-critically stressed due to the diversly-oriented, interconnected faults, which serve to lock one another up. When rupture occurs, typically on a “Keystone fault” (Fletcher et al., 2016, Nature Geoscience), the ruptures can propagate from one fault plane to the next, leading to a complex and sometimes long-lasting earthquake sequence.