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Virginia Polytechnic Institute and State University

Carbonate ramp to deeper shale-shelf transitions of an Upper Cambrian (Dresbachian) shelf embayment, Nolichucky Formation, southwest Virginia

Abstract

dc:description.abstract

The Nolichucky Formation (0-300 m thick) formed as a transgressive-regressive package on the Cambrian pericratonic shelf in a broad, deep water embayment, bordered to the northeast and southeast by peritidal Honaker and Elbrook carbonates. Lateral facies changes from deep embayment rocks to peritidal carbonates suggest that the shelf embayment was bordered by a gently sloping carbonate ramp. Peritidal facies are cyclic, upward-shallowing stromatolite sequences. These grade seaward into subtidal thick, cross-bedded ooid and oncolitic intraclast-grainstones that pass into subwave base deeper ramp nodular dolomottled ribbon carbonates and rare thin lenses of conglomerate. Ribbon limestones are layers and lenses of trilobite packstone, parallel and wave-rippled laminated quartzose calcisiltite and lime mudstone that occur in stormgenerated fining-upward sequences (1-5 cm thick) and as burrowed units. Deeper embayment facies are green, calcareous shale with open marine biota; storm and tidal-current deposited parallel to hummocky laminated, calcareous siltstone; flat pebble conglomerate and rare paraconglomerate (10-60 cm thick) with clasts of deeper water lithologies (storm-lag, debris-flow, or other subaqueous gravity flow deposits); and shaly packstone/wackestone with trace fossils, glauconite horizons, hardgrounds, and erosion/truncation surfaces. A 15 m thick tongue of cyclic carbonates within the shale package contains subtidal calcareous algal, digitate "stromatolite” bioherms and ooid packstones which suggest a period of shoaling in the embayment. Understanding the genesis of these lithofacies may help interpretation of similar rocks that are widely distributed in North American Cambrian and Ordovician units elsewhere.

Degree

thesis:*
Name thesis:degree_name
M. S.
Level thesis:degree_level
masters
Discipline thesis:degree_discipline
Geological Science
Department dc:contributor.department
Geological Science
Grantor dc:publisher
Virginia Polytechnic Institute and State University
Year dc:date.issued
1979

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Markello, James Ross

Rights

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

Identifiers

dc:identifier.*
Handle dc:identifier.uri
https://hdl.handle.net/10919/118885
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/118885

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

Markello, James Ross. Carbonate ramp to deeper shale-shelf transitions of an Upper Cambrian (Dresbachian) shelf embayment, Nolichucky Formation, southwest Virginia. masters thesis, Virginia Polytechnic Institute and State University, 1979. https://hdl.handle.net/10919/118885