Abstract
A pressure wave, initiated by water loading and propagating downward through subsurface water contained in fractures, has been hypothesized as a mechanism for triggering earthquakes along pre-existing faults at depths up to 15-20 km. Such a triggering wave might evidence itself by a coincident wave of descending seismicity. In the New Madrid region, seismicity has been reported to correlate with river stage, but usually with a lag of one to several months. River stage data from New Madrid and earthquake data from the St Louis University's microseismic network were examined for evidence of a time-lag in seismic activity with depth during the interval from Jan. 1, 1978, to May 31, 1987. No evidence for a seismicity wave was found. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 285-288 |
| Number of pages | 4 |
| Journal | Seismological Research Letters |
| Volume | 59 |
| Issue number | 4 |
| Publication status | Published - 1988 |
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)