HR: 0830h
AN: S41C-0087 [PDF]
TI: An Independent Test of the Load/Unload Response Ratio Proposed Method of Earthquake
Prediction
AU: * Trotta, J E
EM: Julie_Trotta@brown.edu
AF: Brown University, Dept. of Geological Sciences, Providence, RI 02912-1846 United States
AU: Tullis, T E
EM: Terry_Tullis@brown.edu
AF: Brown University, Dept. of Geological Sciences, Providence, RI 02912-1846 United States
AB:
It has often been hypothesized that earthquakes should occur more frequently during times of increasing tidal stress, yet the
most careful studies suggest that the effect is very small and difficult to detect. However, as the tectonic stresses rise
and approach failure, tidal stress variations might be more likely to raise the total stress to the failure level. Thus, the
sensitivity of small earthquakes to the tidal stress before an impending large shock might be increased. This idea has been
developed into the Load/Unload Response Ratio (LURR) proposed method of earthquake prediction (Yin et al., 1995). The LURR
method involves looking at the ratio of the number or some measure of the size of small earthquakes that occur during loading
of the tidal cycle to that measure of earthquakes that occur during unloading of the tidal cycle, and suggests this ratio
should increase before an impending large shock. Smith and Sammis (2001, 2003) concluded that there was no predictive
significance to the LURR method, and to our knowledge, this method has not been validated by any independent researchers.
We calculated LURR values for several large earthquakes in southern California, using the methods and parameters described by
Yin et al. (2000) and estimates of the other necessary methods and parameters that were not published. We employed tidal
stresses, both from the solid earth tides alone and together with tidal ocean loading, using programs provided by Agnew
(1996). Increases in the LURR value do occur, but they do not occur more often prior to large earthquakes than at any other
time. We also calculated LURR values for altered datasets in which we randomized the times of each small earthquake before
calculating the tidal stresses, theoretically eliminating any real influence of the tides on LURR. There is no statistically
significant difference between preliminary results from the calculations utilizing the actual earthquake times and
calculations utilizing the randomized times. After considering our results and those of Smith and Sammis (2001, 2003), we
conclude that the LURR method is not a useful tool in earthquake prediction.
DE: 7223 Seismic hazard assessment and prediction
DE: 7260 Theory and modeling
DE: 8194 Instruments and techniques
SC: Seismology [S]
MN: 2003 Fall Meeting