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Virginia Polytechnic Institute and State University

Petrology of the Ashe Formation, Shortt's Knob area, Floyd County, Virginia

Abstract

dc:description.abstract

A small area within the Ashe Formation has been mapped at the scale 1:6000 and studied petrographically and chemically. The rocks have been metamorphosed into the lowermost amphibolite facies and folded. The gross structure is homoclinal, generally N 80° E, >50°SE. Amphibolites (39%), chlorite schists (8%), and quartzofeldspathic schists and gneisses (53%) are the major lithologies. Amphibolite assemblages are hornblende + clinozoisite and/or epidote + plagioclase + sphene ± quartz ± garnet. Amphibolites may be divided into four types on the basis of texture, sphene-content, and epidote-composition. Chlorite schists are ultrabasic rocks containing the assemblage Mg-chlorite + actinolite and/or cummingtonite + dolomite + ilmenite ± olivine. Metasediments generally contain biotite. The most distinctive metasediment is black sulfidic schist containing 15-20% amorphous carbon. The assemblage dolomite + quartz + muscovite + plagioclase + biotite occurs in the only carbonate outcrop. Anorthite content of plagioclase ranges between 18 and 40 mol % but depends on lithology. Amphibolite hornblendes have at least one A1<sup>IV</sup> per formula unit. Epidote group minerals have compositions generally <Ps₅ or >Ps₁₀ and the concept of a single miscibility gap is not supported. Upper P-T limits will be defined by the reaction dolomite + quartz + muscovite -> plagioclase + biotite + calcite + vapor and probably limit the temperature to <550°C. The reaction zoisite + CO₂ -> anorthite + calcite + H₂O limits the CO₂ content of the metamorphic fluid over most of the area to low values, probably <0.1 mol fraction. The amphibolites probably represent basaltic flows, some amygdaloidal. Chlorite schists are interpreted to have been picritic sills.

Degree

thesis:*
Name thesis:degree_name
M.S.
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
1973

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Davison, William Donald

Rights

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

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/10919/91115
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/91115

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
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citation

Davison, William Donald. Petrology of the Ashe Formation, Shortt's Knob area, Floyd County, Virginia. masters thesis, Virginia Polytechnic Institute and State University, 1973. http://hdl.handle.net/10919/91115