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Virginia Polytechnic Institute and State University

Structural evolution of the Max Meadows thrust sheet, Southwest Virginia

Abstract

dc:description.abstract

Fold and fault structures in sub-greenschist strata of the most internal, Southern Appalachian foreland thrust sheet developed in progressive simple shear near the ductile-to-brittle transition. Heterogeneous simple shear (γ < 3) was localized in incompetent, anisotropic pelitic rocks (Rome Formation) along the base of a composite, 5-11 km. thick thrust sheet. Folds, which vary from upright and open to isoclinal and strongly overturned, developed during ductile shearing and display a correlation between tightness and axial surface orientation. Deformation culminated by movement along brecciated thrust zones which evolved progressively from zones of greatest ductile strain. This resulted in low angle truncation of fold axis trends and approximately coaxial refolding of earlier structures. PhyIlosiIicate recrystallization during ductile folding and cleavage formation records the thermal maximum (200-300+°C). Syntectonic veins indicate that fluid pressures (P<sub>f</sub>) in excess of only the minimum compressive stress prevailed during ductile deformation. Increasing fluid pressures and/or decreasing confining pressures (P<sub>c</sub>) eventually led to hydrofracturing and, possibly, fault initiation in pelitic strata. Fault rock morphology is largely lithology dependent; most breccias developed by refolding, cataclasis, and later dedolomitization of previously cleaved, veined, and boudinaged, anisotropic strata. Significant intracrystalline strain indicates conditions near the quasiplastic elastico-frictional transition during fault initiation. Changing physical conditions (decreasing temperature and increasing P<sub>f</sub> : P<sub>c</sub>) during deformation resulted in the transition from ductile folding to brittle thrusting. These changes may reflect erosional unroofing during uplift and thrust sheet emplacement.

Degree

thesis:*
Name thesis:degree_name
M.S.
Level thesis:degree_level
masters
Discipline thesis:degree_discipline
Geology
Department dc:contributor.department
Geology
Grantor dc:publisher
Virginia Polytechnic Institute and State University
Year dc:date.issued
1983

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Gibson, R. G. (Richard G.)

Rights

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

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/10919/114410
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/114410

Chain of custody

source
Harvested from
Virginia Tech
Base URL
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Last updated
2026-07-22
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citation

Gibson, R. G. (Richard G.). Structural evolution of the Max Meadows thrust sheet, Southwest Virginia. masters thesis, Virginia Polytechnic Institute and State University, 1983. http://hdl.handle.net/10919/114410