The Norcross Gneiss of the Atlanta Group, here named in the Newnan-Tucker synform near Atlanta, GA, consists of well-foliated gray, epidote-biotite-muscovite-plagioclase gneiss with pods and lenses of amphibolite. It is in sharp contact and correlative with the Wolf Creek Formation to the southwest; it is gradational and conformable with the overlying Clairmont Formation. 2,000 m thick. Age is Late Proterozoic and (or) early Paleozoic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Norcross Gneiss is removed from the Atlanta Group, here abandoned. It is a granitic sill in the Clairmont thrust sheet which separates the main mass of the Clairmont melange from the lower part, which was formerly named the Inman Yard Formation but is now known to be part of the Clairmont Formation. The Norcross is interpreted to be a remnant of a subduction melange associated with the volcanic arc in which rocks in overlying thrust sheets formed. Age is Silurian(?).
Source: GNU records (USGS DDS-6; Reston GNULEX).
Recent mapping has shown Norcross Gneiss to be a facies of Lithonia Gneiss. Because Lithonia is a well-established name and takes precedence over Norcross, Norcross Gneiss is herein abandoned.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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