Linking fossil reefs with earthquakes: geologic insight to where induced seismicity occurs in Alberta
Faculty Advisor
Date
2016
Keywords
induced seismicity, Western Canada Sedimentary Basin
Abstract (summary)
Recently, a significant increase in North American, midcontinent earthquakes has been associated
with contemporaneous development of petroleum resources. Despite the proliferation of drilling throughout
sedimentary basins worldwide, earthquakes are only induced at a small fraction of wells. In this study, we focus
on cases of induced seismicity where high-resolution data are available in the central Western Canada
Sedimentary Basin. Our regional comparison of induced earthquake depths suggests basement-controlled
tectonics. Complementary to these findings, hypocenters of induced seismicity clusters coincide with the
margins of Devonian carbonate reefs. We interpret this spatial correspondence as the result of geographically
biased activation potential, possibly as a consequence of reef nucleation preference to paleobathymetric highs
associated with Precambrian basement tectonics. This finding demonstrates the importance of geologic/tectonic
factors to earthquake induction, in addition to industrial operational parameters. In fact, the observation of
induced seismicity silhouetting deep fossil reef systems may be a useful tool to identify future regions with
increased seismogenic potential.
Publication Information
Schultz, Ryan, Hilary Corlett, Kristine Haug, Ken Kocon, Kelsey MacCormack, Virginia Stern, and Todd Shipman. "Linking fossil reefs with earthquakes: Geologic insight to where induced seismicity occurs in Alberta." Geophysical Research Letters 43, no. 6 (2016): 2534-2542.
Notes
Item Type
Article
Language
English
Rights
Attribution-NonCommercial-NoDerivs (CC BY-NC-ND)