Manga and Bordsky 26 reported that both static stress change and dynamic stress may be significant in the near field and intermediate field (i.e., within up to a few fault lengths), but only dynamic stress is larger than tidal stress in the far field (i.e., many fault lengths away).
← all excerpts
Effective time- and frequency-domain techniques for interpreting seismic precursors in groundwater level fluctuations on Jeju Island, Korea.
1
—
—