By analyzing seismicity induced by the injection of wastewater into the Costa Molina 2 well, we characterized attenuation in the area. Attenuation quality factors Q P and Q S were calculated using the peak-frequency method, which is suitable for small-magnitude earthquakes registered in the region.
Anomalously high attenuation with values of effective Q(P) similar to 48 and Q(P) / Q(S) ratio of less than 1 in the vicinity of the injection well was found, in comparison with Q(P) similar to 60 for the rest of the region. Furthermore, the V-P / V-S ratio was also found to be high in the close vicinity of the injection well.
We determine how sedimentary rocks possibly change their geomechanical properties due to salt-water injection and find that observed changes of attenuation (increase) and V-P / V-S ratio (increase) are consistent with the geomechanical models and experiments. Our findings indicate that the observed anomaly in the vicinity of the Costa Molina 2 well is due to the (1) changes of the properties of the rock mass affected by injection and (2) 3D structure in the overburden rocks.