The Fairburn Member is here named the lower member of the Clarkston Formation of the Atlanta Group in the area from East Point to Palmetto, GA, in the northwest limb of the Newnan-Tucker synform. It consists of crinkled garnet schist and locally contains small red garnets. Overlies the Stonewall Formation with sharp and conformable contact; gradationally underlies the Tar Creek Member of the Clarkston. Thickness is 400 to 1,000 m. Age is Late Proterozoic and (or) early Proterozoic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Fairburn Member of the Clarkston Formation occurs in the Clarkston slice of the Atlanta thrust sheet. Age is Late Proterozoic to Early Ordovician(?).
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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