Time histories of seismic attenuation from the San Andreas fault at Parkfield
During the seismic cycle, in nature and as well as in lab samples, the crack density of
rocks varies substantially, as stressed rocks approach a critical state and eventually
fail (Vasseur et al, 2017; Nur, 1972; Gupta, 1973) . At Earth scales, small periodical stress variations such
as seasonal loading/unloading and tides (Johnson_etal_2017) are constantly being superimposed
on the tectonic loading stress of crustal rocks, inducing periodic changes in crack
porosity, pore-fluid pressure, and saturation, that should leave a signature on crustal
attenuation.