http://smu.edu/newsinfo/pdf-files/earthquake-study-10march2010.pdf...
Following the October earthquakes, seismologists from Southern Methodist University (SMU) borrowed six, three-component, broadband seismographs from an NSF-supported instrument pool and operated them at sites in Tarrant and Dallas Counties (Figure 2) between 9 November 2008 and 2 January 2009. Although the NEIC reported no felt earthquakes during this period, the SMU stations recorded numerous local events, including 11 earthquakes between 20 November and 2 December with exceptionally well-recorded P and S arrivals on three stations, AFDAD, AFMOM, and CPSTX.
The present paper summarizes our analysis of seismograms of the DFW sequence and reports precise locations for 11 well-recorded but “non-felt” events. Using seismological data and other information available in the public record, we show that: (1) In 2008 prior to 29 October, we detected no earthquakes occurring near DFW, including earthquakes too small to be locatable by the NEIC; (2) the 11 hypocenters have a preferred focal depth of 4.4 km and lie along a 1.1 km SW-NE line; and (3) the mean epicenter estimate of the 11 events is less than 0.5 km from a 4.2-km deep saltwater disposal (SWD) well where injection began on 12 September 2008, seven weeks before the DFW focus became active. On the basis of time and spatial correlations, we conclude the DFW sequence may be the result of fluid injection at the SWD well, but we are puzzled as to why earthquakes occur at this particular location but not near other SWD wells in the region. Finally, we discuss the DFW earthquakes in the context of regional historical seismicity, which includes both natural and induced earthquakes. We observe that historical induced earthquakes in the Texas region have all been less than magnitude 4.6 and have not produced substantial damage.
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Acknowledgments: We thank the Incorporated Research Institutions for Seismology (IRIS) instrument pool for providing the seismographs used in this study. We gratefully acknowledge discussions with scientists at Chesapeake Energy concerning regional geology, brine injection practices, and regional seismicity.