The Appling granite is a post-metamorphic granitic pluton of Permian age. It is undeformed by Appalachain stress and strain with an age of 294 Ma. It is one of the youngest intrusions in the southern Appalachian Piedmont. It has intruded the Kiokee belt. Stop 7 Dennis.
References
Page 48 - Dennis, A.J., 2016, Structural analysis of the Kiokee belt and its framing elements: Savannah River transect: Geol. Soc. Am. Field Guide 42, p. 37-51.
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