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Vidale would like to see measurements of how much deformation occurs above the deep tremors using GPS or radar imagery.
This value is approximately the same as for the case of deep tremors in the Kii Peninsula.
Note that the value is two orders of magnitudes smaller than the migration speed of non-volcanic deep tremors.
Nadeau has also recently found a correlation between the deep tremors and small earthquakes, magnitude 2 or smaller, closer to the surface.
In 2012, scientists spotted deep tremors on the San Andreas fault below Parkfield that were tidally triggered, at the twice-a-day tidal peaks associated with the lunar day.
This value of diffusivity is also consistent with the migration of non-volcanic deep tremors in western Shikoku, south-west Japan (Ide 2010), for which fluid likely plays an important role.
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Van der Elst says that the daily tidal peaks seem to trigger the littlest, deepest tremors, whereas the larger spring tide sets off larger patches of slip higher up.
Mysterious tremors normally associated with volcanic activity have been detected deep on the San Andreas fault in California.
A Widow Left With Grief Months later, some of the survivors were still struggling with deep emotional tremors.
It has been reported that slow earthquakes including slow slips, deep episodic tremors, and low-frequency earthquakes are shear slips with long characteristic source durations that radiate less seismic energy (e.g., Hirose et al. 1999; Ito et al. 2006; Obara 2002); this suggests that they have small stress drops.
Deep tectonic tremors are small-amplitude, long-lasting seismic events that occur in a belt-like zone at around 20- to 40-km depth and have been observed in various tectonic regions since their first discovery in southwestern Japan by Obara (2002).
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