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Virginia Polytechnic Institute and State University

Kinematic analyses of discfolds in Devonian Millboro Formation in the Central-Southern Appalachian junction zone

Abstract

dc:description.abstract

A method of kinematic analysis has been applied to discfolds in the Devonian Millboro Formation in the junction zone and adjacent, differently trending segments of the Central and Southern Appalachian Valley and Ridge Province. Types and kinematic signatures of shearing movements that produced discfolds at twenty localities have been recognized. Discfolds are a type of flexural fold produced by planar shearing movements during northwestern translation and deformation of the Paleozoic cover, and their analyses reflect the orientations of the large-scale movements that produced the major folds and faults. Most analyses indicate northeast-striking, southeast-dipping slip planes, northwest-trending slip lines, and overall vergence of the shear zones to the northwest. Discfolds on northwest limbs of major anticlines were produced by shearing along late-stage, southeast-dipping reverse faults, and those on the southeast limbs by shearing along southeast-dipping, bedding-parallel reverse faults and/or by large-scale flexural flow. Analyses of discfolds in the junction zone indicate movement of material out of the zone toward both the northeast and southwest. Visual and statistical comparisons between analyses of the central and southern segments show contrasts in the orientations of the slip planes and slip lines. Thus, the transport directions of the two segments converged toward the northwest, and are consistent with those that must have operated earlier in the formation of the major folds and faults. This conclusion coupled with the apparently similar timing of the discfolds indicates that there was, at most, only slight northwestern rotation of the southern segment in relation to the central.

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
1977

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Stubbs, John Latham

Rights

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

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/10919/74125
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/74125

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

Stubbs, John Latham. Kinematic analyses of discfolds in Devonian Millboro Formation in the Central-Southern Appalachian junction zone. masters thesis, Virginia Polytechnic Institute and State University, 1977. http://hdl.handle.net/10919/74125