An investigation of seismicity clustered near the Cordel Field, west central Alberta, and its relation to a nearby disposal well

Historically, seismicity documented in the Western Canada Sedimentary Basin has been relatively quiescent and earthquakes are usually restricted to the foreland belt of the Rocky Mountains. However, exceptional clusters of events, which have remained active for decades, are recognized in Alberta. In...

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Bibliographic Details
Published in:Journal of geophysical research. Solid earth 2014-04, Vol.119 (4), p.3410-3423
Main Authors: Schultz, Ryan, Stern, Virginia, Gu, Yu Jeffrey
Format: Article
Language:English
Subjects:
Alberta
Analysis
Brazeau cluster
Clusters
Earthquakes
Fluid injection
Geophysics
Induced seismicity
Injection
Mountains
Plate tectonics
Pumping rates
Sedimentary basins
Seismic activity
Seismic phenomena
Seismicity
Seismology
Stations
Statistical analysis
Waste water
Waste water disposal
Wastewater
Waveforms
Western Canada Sedimentary Basin
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Summary:Historically, seismicity documented in the Western Canada Sedimentary Basin has been relatively quiescent and earthquakes are usually restricted to the foreland belt of the Rocky Mountains. However, exceptional clusters of events, which have remained active for decades, are recognized in Alberta. In this study we investigate the seismicity in this region using data obtained from recently established regional arrays, emphasizing the relationship between a disposal well in the Cordel Field and a nearby cluster of previously reported earthquakes. We explore temporal correlations of wastewater pumping rates and local seismic activity dating back to 1960. We find that the first statistically significant increase in seismicity lags the onset of wastewater injection (October 1991) by ~3.33years. In particular, the waveform similarity of 32 events are analyzed from continuous data recorded at NOR, a nearby (~30km) station operated by the University of Alberta starting in September of 2006. Results from this analysis suggest that many events are well correlated in the characteristics of the waveforms and thus are likely to share a similar origin and source mechanism. The most prolific of these multiplets repeats more than 10 times sporadically throughout the entire duration of recorded data from October 2006 to March 2012. Despite the limited availability of nearby stations, which adversely affects the resolution of our analysis, hypocenter depths could be relatively accurately determined from waveform synthesis and double difference methods. The results of our analysis provide first-order evidence that the seismicity is consistent with fluid injection-induced events. Key Points * A cluster of events is investigated and found to be induced
ISSN:2169-9313
2169-9356
DOI:10.1002/2013JB010836