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Virginia Tech

High pressure acadian metamorphism of the Straits Schist, Western Connecticut

Abstract

dc:description.abstract

A detailed petrologic study of the maximum assemblage, minimum variance pelitic units contained within The Straits Schist in western Connecticut was undertaken to provide data on the Acadian Orogeny in the northern half of the western highlands of Connecticut. The Straits Schist, contained within the Connecticut Valley synclinorium, is structurally involved in portions of both the Hartland and Gneiss Dome belts, outlining isoclinally refolded nappes plunging off the Waterbury Dome. The Straits Schist is believed to be of Silurian—Devonian age, based on proposed correlations with the Goshen and the Waits River Formations of Massachusetts and Vermont, respectively. Furthermore, the age of metamorphism is interpreted as being Acadian based on the proposed age and stratigraphy, simple metamorphic textures, and uniform grain sizes. Quantitative estimates of the pressure and temperature conditions under which the mineral assemblages of The Straits Schist equilibrated were calculated using calibrated mineral reactions and ion exchange equilibria. Temperatures range from 607° — 747°C, and pressures range from 6.4 — 8.9 kbar across the study area. Estimates of P<sub>H₂0</sub>/P<sub>total</sub> were obtained and range between 0.21 and 0.57. Although exchange mechanisms have not (or could not have) been determined exactly, biotite and muscovite do show deviation from ideal tri- and di-octahedral stoichiometry, up to 13.7% di-octahedral character and 2.2% tri-octahedral character, respectively. Compositional X-ray maps indicate that The Straits Schist underwent rapid cooling. Therefore, the Acadian Orogeny in western Connecticut is characterized as a high-pressure event that underwent rapid postmetamorphic uplift and cooling.

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 Tech
Year dc:date.issued
1990

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Miller, Stephen John

Rights

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

Identifiers

dc:identifier.*
Dc Identifier Other
etd-03242009-040839
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/41784

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

Miller, Stephen John. High pressure acadian metamorphism of the Straits Schist, Western Connecticut. masters thesis, Virginia Tech, 1990. http://hdl.handle.net/10919/41784