TY - JOUR
T1 - Hydroseismicity - a viable trigger mechanism in the New Madrid seismic zone?
AU - Ervin, C. P.
AU - El-Hussain, I.
PY - 1988
Y1 - 1988
N2 - 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
AB - 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
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U2 - 10.1785/gssrl.59.4.285
DO - 10.1785/gssrl.59.4.285
M3 - Article
AN - SCOPUS:0024224111
SN - 0895-0695
VL - 59
SP - 285
EP - 288
JO - Seismological Research Letters
JF - Seismological Research Letters
IS - 4
ER -