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Virginia Polytechnic Institute and State University

The Fries Fault near Riner, Virginia: an example of a polydeformed, ductile deformation zone

Abstract

dc:description.abstract

The Fries Fault, a 1.2-2.3 km wide zone near Riner, is a major tectonic discontinuity in the Blue Ridge geologic province, characterized by progressive stages of continuous ductile deformation. Trending northeast with a shallow to moderate southeast dip, this fault juxtaposes Little River Gneiss on the southeast against Pilot Gneiss and the Chilhowee Formation to the northwest. A 0.8-1.2 km wide subzone of protomylonite within the Little River Gneiss grades into a 0.5-1.0 km wide mylonite subzone, the latter containing narrow bands of phyllotactic ultramylonite ranging in width from centimeters to tens of meters. Mylonitization is reflected by a marked reduction in grain size, elongation of quartz and fracturing of feldspar, all concomitant with the development of a mylonitic foliation (S<sub>m</sub>). Ductile deformation processes involving grain elongation, recovery and recrystallization, combined with chemical processes (primarily pressure solution), are the dominant strain-accommodation mechanisms in the formation of S<sub>m</sub>. Rocks within the fault zone have undergone four phases of Paleozoic deformation. An early S₁ foliation has been nearly completely transposed by S<sub>m</sub>(S₂), which dominates across most of the area. The development of S<sub>m</sub> was accompanied by a retrogressive metamorphism that altered basement rocks from lower amphibolite to greenschist facies. Chilhowee Group rocks remained at lower greenschist facies. Post-faulting deformation produced an S₃ crenulation cleavage associated with northeast trending, overturned F₃ folds. Subsequent refolding produced open, northwest trending F₄ folds. Although the bulk deformation is progressive simple shear, flattening is increasingly dominant during the later stages of deformation.

Degree

thesis:*
Name thesis:degree_name
Master of Science
Level thesis:degree_level
masters
Discipline thesis:degree_discipline
Geological Sciences
Department dc:contributor.department
Geological Sciences
Grantor dc:publisher
Virginia Polytechnic Institute and State University
Year dc:date.issued
1979

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Kaygi, Patti Boyd

Rights

dc:rights
Statement dc:rights
  • In Copyright
Language dc:language.iso
en_US

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/10919/53821
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/53821

Chain of custody

source
Harvested from
Virginia Tech
Base URL
vtechworks.lib.vt.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
related terms
citation

Kaygi, Patti Boyd. The Fries Fault near Riner, Virginia: an example of a polydeformed, ductile deformation zone. masters thesis, Virginia Polytechnic Institute and State University, 1979. http://hdl.handle.net/10919/53821