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Virginia Polytechnic Institute and State University

Major element and isotopic studies on the James Run/Port Deposit association, Maryland: tectonic analogues and Taconic deformation

Abstract

dc:description.abstract

The gneissic Port Deposit pluton and associated James Run metavolcanics bear a fault relation with the Wissahickon metasediments of the Glenarm terrane of the northeastern Maryland Piedmont, USA. Bulk chemical and mineralogical data classify the meta-igneous rocks as a bimodal tholeiite-dacite/tonalite suite with trondhjemitic affinities and indicate that subsolidus alteration during dynamic metamorphism was minor. Comparison of these data with other tectonic environments suggests their generation by partial fusion of amphibolitic basement. Previous studies have dated magmatic events in the Maryland Piedmont at 520 Ma, 420 Ma, and 300 Ma (Sinha et al., 1980). The U-Pb zircon upper intercept age for the Port Deposit is 525 ± 10 Ma, the Rb-Sr whole rock isochron age is 467 ± 21 Ma, and Rb-Sr model biotite ages are 400 and 300 Ma. Regional and theoretical considerations indicate the 525 zircon age may represent the time of igneous consolidation. Detailed petrographic observations in the Port Deposit indicate the Rb-Sr whole rock age represents the time of deformation and development of gneissic textures. The 467 Middle Ordovician age of deformation for the Port Deposit is interpreted as representative of the Taconic orogeny for the central Appalachian Piedmont; Rb-Sr whole rock systematics were upset, but concurrent anatexis of felsic basement is not locally evident. The fault contact between the Port Deposit and easternmost facies of the Wissahickon places an upper age limit of 467 Ma for that particular facies. Rb-Sr model biotite ages are interpreted as metamorphic cooling phenomenon and reflect the 420 and 300 Ma thermal highs.

Degree

thesis:*
Name thesis:degree_name
Master of Science
Level thesis:degree_level
masters
Discipline thesis:degree_discipline
Geology
Department dc:contributor.department
Geology
Grantor dc:publisher
Virginia Polytechnic Institute and State University
Year dc:date.issued
1982

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Lesser, Richard Peter

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/10919/80237
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/80237

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

Lesser, Richard Peter. Major element and isotopic studies on the James Run/Port Deposit association, Maryland: tectonic analogues and Taconic deformation. masters thesis, Virginia Polytechnic Institute and State University, 1982. http://hdl.handle.net/10919/80237