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Virginia Polytechnic Institute and State University

The gravity field over the Bane Dome in Giles County, Virginia

Abstract

dc:description.abstract

The Bouguer gravity field, deterrmined from 395 measurements in Giles County, Virginia exhibits a broad positive anomaly approximately 12 mgal in amplitude situated over the Bane Dome, and several smaller anomalies of a few milligals amplitude. For the most part they are produced by the distribution of relatively high density carbonate rocks and lower density clastic rocks within the dome. These anomalies can be explained by two contrasting interpretations of the structure of the Bane Dome. One interpretation, represented by the geologic cross sections of Woodward and Gray (Woodward, 1985) and Bartholomew (personal communications, 1987) suggests that the dome is cored by a relative abundance of high density carbonate rocks transported by overthrusting within the Narrows thrust sheet. Because the gravity anomalies can be entirely explained by sources confined to the Narrows thrust sheet, this interpolation precludes the existence of significant lateral density contrasts associated with deeper structure beneath the decollement zone in the Rome Formation. The contrasting interpretation represented by the cross section of Gresko (1985), suggests a smaller proportion of carbonate rocks in the core of the dome due to duplex structures in the lower density clastic rocks. This interpretation proposes high angle faults with associated lateral density contrasts in the deeper rocks underlying the decollement. Because sources within the Narrows thrust sheet are insufficient to completely account for the gravity anomalies, the density contrasts associated with deeper structure are required. The Bouguer gravity field can be separated into regional and residual parts. The regional field is caused by changes in crustal thickness known independently from the seismic measurements of James, Smith, and Steinhart (1968). The remaining residual field can be explained in terms of anomaly sources within the upper 10 km of the crust.

Degree

thesis:*
Name thesis:degree_name
Master of Science
Level thesis:degree_level
masters
Discipline thesis:degree_discipline
Geophysics
Department dc:contributor.department
Geophysics
Grantor dc:publisher
Virginia Polytechnic Institute and State University
Year dc:date.issued
1988

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Moses, Michael J.

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/10919/53176
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/53176

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

Moses, Michael J.. The gravity field over the Bane Dome in Giles County, Virginia. masters thesis, Virginia Polytechnic Institute and State University, 1988. http://hdl.handle.net/10919/53176