Back to results

Virginia Polytechnic Institute and State University

Polyphase deformation and metamorphism in the Penobscot Bay Area, Coastal Maine

Abstract

dc:description.abstract

Metasediments from portions of two of the six lithologic terranes in the Penobscot Bay area of coastal Maine, the Late Precambrian (?) to Ordovician(?) Copeland Formation and the Rider Bluff member of the Copeland Formation at the eastern margin of the Passagassawakeag (PGW) terrane and the Silurian (?) to Devonian (?) Bucksport Formation of the adjacent Bucksport terrane, shared a common history of four phases of ductile deformation (D₁, D₂, D₃, and D₄) and interdeformational metamorphism and granitic plutonism. D₁ (early Acadian ?) produced tight to isoclinal folds and an axial plane foliation that deform all three metasedimentary units and contacts between these units. These units and therefore the PGW and Bucksport terranes must have been together by the time of D₁ at the latest. No observed structural or metamorphic gradient coincides with this terrane boundary in the Penobscot Bay area, but in southeast Maine it is mapped as a pre-metamorphic thrust fault. Intrusion of the 412± 14 Ma Stricklen Ridge granite and amphibolite facies metamorphism occurred between D₁ and D₂ . D₂ (Acadian) produced open, upright folds and a strong, hinge-parallel mineral elongation lineation under upper greenschist to lower amphibolite conditions. D₃ ductile strike-slip shear zones formed under upper greenschist to lower amphibolite conditions, and D₄ open, steeply-reclined folds formed under greenschist facies conditions. D₃ and D₄ are probably related to the same stress system as the dextral strike-slip Norumbega Fault Zone (Alleghanian) and probably represent a continuum of deformation. Brittle faults exploit D₃ shear zones and may also be related to the same stress system.

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
1986

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Kaszuba, John Paul

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/10919/91036
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/91036

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

Kaszuba, John Paul. Polyphase deformation and metamorphism in the Penobscot Bay Area, Coastal Maine. masters thesis, Virginia Polytechnic Institute and State University, 1986. http://hdl.handle.net/10919/91036