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National Geologic Map Database
Geologic Unit: Bassett
Map showing publication footprint
  • Usage in publication:
    • Bassett Formation
  • Modifications:
    • Named
  • Dominant lithology:
    • Gneiss
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Map showing publication footprint
  • Usage in publication:
    • Bassett Formation
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Horton, J.W., Jr., and McConnell, K.I., 1991, The western Piedmont, IN Horton, J.W., Jr., and Zullo, V.A., eds., The geology of the Carolinas: Carolina Geological Society, 50th Anniversary Volume, p. 36-58.


Summary:

In southern VA, Bassett Formation of Conley and Henika (1973) is physically lowest formation and interpreted as oldest unit in the Smith River allochthon. Consists of a lower biotite gneiss member and an upper amphibolite member. Lower unit is fairly homogeneous, medium-grained, and generally very thinly layered with zones of migmatite and pods and lenses of ultramafic rock and thin metagabbro bodies. Units mapped in NC by Lewis (1980) as "felsic gneiss mixed with biotite gneiss" and as "biotite gneiss" may be equivalent to the biotite gneiss member of the Bassett Formation. Amphibolite member thins to the southwest and is not abundant in NC. Underlies Fork Mountain Formation.

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.

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