This article describes an unusually well-behaved, unusually well-documented central and eastern United States (CEUS) earthquake sequence. Detailed analysis of regional and local waveform data from the 6 June 2003 Bardwell, Kentucky, earthquake indicates that the mainshock has the seismic moment of M-0 1.3 (&PLUSMN; 0.5) x 10(15) N m (M-w 4.0) and occurred at a depth of about 2 (&PLUSMN; 1) km on a near-vertical fault plane. A temporary seismic network recorded 85 aftershocks that delineate an east-trending fault approximately I km in length. The hypocenters illuminate a vertical plane between 2.0 and 2.7 km depth. The centroid of the aftershock distribution is at 36.875&DEG; N, 89.010&DEG; W and a depth of 2.4 km. The aftershock cluster is interpreted as a circular fault area with a radius of 0.44 (&PLUSMN; 0.03) km. This source radius yields a static stress drop, &UDelta;σ = 67 (&PLUSMN; 14) bars for the mainshock. The focal mechanism for the mainshock has strike 90&DEG;, dip = 89&DEG;, and rake = -165&DEG; with a subhorizontal P axis trending 135&DEG;. A formal stress inversion based on the focal mechanisms of the mainshock and ten aftershocks indicates the maximum compressive stress trends 104&DEG; with a plunge of 5&DEG;. The local stress field near Bardwell is therefore rotated about 40&DEG; clockwise relative to 65&DEG; for eastern North America as a whole. The Bardwell earthquakes have the opposite sense of slip to earthquakes with east-trending nodal planes that occur near New Madrid, Missouri. This requires a significant local rotation of the stress field over a distance of 60 km.
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