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Seismicity and tectonics of the Garfield Hills area Nevada
(University of Nevada, Reno, 1989)
The seismicity and tectonics of the Garfield Hills area have been studied. The seismicity of the area sometimes correlates with mapped faults, and is characterized by short-lived, randomly distributed clusters.
A preliminary study of focal mechanisms of small earthquakes in the central Nevada region
(University of Nevada, Reno, 1967)
First arrivals suggest that normal and right-lateral movement was occurring on the Fairview Fault, except at the southern end, where it appears that reverse faulting is occurring.