Clark (1987) identified, on 12-fold Vibroseis data, five seismic anomalies, which he associated with paleotopographic lows in the Mississippian. These anomalies, in conjunction with a Morrowan depositional model, were used to guide the exploration and development of the Minneola complex subsequent to the initial discovery. In beginning his discussion of the seismic stratigraphy of the area, Clark correctly acknowledged the critical importance of establishing the position of the Mississippian-Pennsylvanian unconformity on the seismic data. Although “approximately 30 synthetic seismograms” (Clark, 1987, p. 1334) were used to do so, Clark has no illustrations of these ties and no comment...
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