New Madrid seismotectonic study. Summary of activities from 1977 through 1981

This report summarizes a five year coordinated program of geological, geophysical, seismological studies in the New Madrid area. The program was designed to define the structural setting and tectonic history of the area in order to realistically evaluate earthquake risks in the siting of nuclear facilities. Interpretation of gravity, magnetic, and seismic reflection investigations in the New Madrid area indicate a spatial correspondence of the seismic activity to an ancient rift. Regional studies show that this rift extends to the southwest and to the northeast where it becomes part of a much more extensive rift complex. Two models have been proposed to account for the interpreted structure and seismicity in the New Madrid area. One model suggests that the ancient rift is a zone of weakness in the crust along which regional, largely horizontal, stresses are relieved. Presumably this has occurred repeatedly throughout the Phanerozoic. Another model has the rift being reactivated by local, largely vertically-derived forces which are derived from a thermal perturbation within the upper mantle. Field studies, drill holes, trenching, seismic surveys, and detailed gravity studies have shown that only small-scale or no movements have occurred along any of the faults studied since the beginning of Quaternary time. However, studies of the geomorphology of the area suggest that minor amounts of warping have occurred in parts of the region since the Pleistocene terraces were formed. Also, faults with displacements of up to 3 meters, folds, and sandblows were identified in a trench excavated across the Tiptonville (Reelfoot) scarp in northwestern Tennessee