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Argues that in the report of Cook et al (Geology, 7, 563-567), there is no conclusive evidence, on the basis of seismic- reflection profiling of the crystalline southern Appalachians, that subhorizontal features revealed at depths of several kms. actually represent flat-lying sedimentary rocks. Offers an alternntive interpretation, suggesting that the features shown by the southeastern Blue Ridge - Piedmont COCORP line represent a flat-lying complex of thin but extensive granitic sheets and associated high rank schist and gneiss. -after Author
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Comment on ' Thin-skinned tectonics in the crystalline southern Appalachians: COCORP seismic- reflection profiling of the Blue Ridge and Piedmont'.