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  • Usage in publication:
    • Laura Lake Mafic Complex
  • Modifications:
    • Named
  • Dominant lithology:
    • Amphibolite
    • Gneiss
    • Gabbro
    • Iron-formation
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

McConnell, K.I., and Abrams, C.E., 1984, Geology of the greater Atlanta region: Georgia Geologic Survey Bulletin, no. 96, 127 p.


Summary:

The largest premetamorphic intrusive-extrusive complex in the Piedmont portion of the Greater Atlanta Region is here named the Laura Lake Mafic Complex of the New Georgia Group. It is a body of migmatitic garnet amphibolite, clinopyroxene, felsic gneiss, metagabbro, meta-ultramafic rocks, and banded iron formation. It is separated from the outcrop belt of the New Georgia Group by a thin strip of Sandy Springs Group rocks. Because of lithologic similarities to the New Georgia, the Laura Lake is believed to represent a slice of the New Georgia that, along with the Sandy Springs, was thrust over other units of the New Georgia.

Source: GNU records (USGS DDS-6; Reston GNULEX).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

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