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Virginia Polytechnic Institute and State University

Regional cementation associated with unconformity-sourced aquifers and burial fluids, Mississippian Newman Limestone, Kentucky

Abstract

dc:description.abstract

Aquifer-related cements may be differentiated from deeper burial cements by trace elements, cathodoluminescence, staining, and fluid inclusion analysis in the Mississippian Newman Limestone, eastern Kentucky. Aquifer cements are nonferroan, and show a nonluminescent to dull to nonluminescent to bright cathodoluminescent zonation. They fill leached ooids and fossils indicating waters initially were undersaturated. Early nonluminescent cement (35 ppm Mn, 35 ppm Fe) formed from oxidizing waters in a regional paleoaquifer that became reducing (dull cement; 180 ppm Mn, 565 ppm Fe) but underwent later recharge to form a second nonluminescent cement. Most cementation appears to have been associated with post-Newman unconformities reflecting a shift to a wetter climate in Late Mississippian-Pennsylvanian time which generated regional aquifers. Aquifer cement abundance decreases away from recharge areas and is determined by staining for late burial calcite and then using image analysis to determine the amount of early unstained cement. Later, iron rich burial cements (780 ppm Mn, 4295 ppm Fe) fill remaining pore spaces, compaction-induced fractures, spalled cement rims and tectonic fractures (lined with saddle dolomite and pyrite). Irregular dull/very dull zone patterns relate to preferential concentration of iron along certain crystal faces rather than burial leaching. Secondary fluid inclusions chemically complex brines suggest late stage fluids were (7-17 wt% NaCl) having minimum temperatures of 51 to 156°C, that resided in the formation for such short times that conodont alteration values (consistent with estimated burial temperatures of 38-40°C) were not affected.

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
1984

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Niemann, James Cottier

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/10919/76196
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/76196

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

Niemann, James Cottier. Regional cementation associated with unconformity-sourced aquifers and burial fluids, Mississippian Newman Limestone, Kentucky. masters thesis, Virginia Polytechnic Institute and State University, 1984. http://hdl.handle.net/10919/76196