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Virginia Polytechnic Institute and State University

Anorthositic sills of the southern Adirondack Mountains of New York state

Abstract

dc:description.abstract

The Speculator Sheet and the Wells-Tenantville Sill are intruded into the Rooster Hill/Little Moose Mountain Formations in the southern Adirondacks. The Wells Sill consists of a medium-grained gabbro forming the top and basal layers, and an inner core of anorthositic gabbro rimmed by a fine-grained chill margin called the Tenantville facies. The Speculator Sheet consists of gabbroic anorthosite and has a mafic lower margin due to gravitational settling of mafic phases. Plagioclase and pyroxene compositions suggest that the Wells gabbro is distinct from the rest of the sills and is related to the Oregon Dome. Whole rock data show that the gabbroic anorthosite and the rocks of the Thirteenth Lake Dome have a differentiation trend of minor iron enrichment, while the Wells gabbro, Oregon Dome and Snowy Mountain Dome have a trend of more extreme iron enrichment. Field evidence indicates that the Wells gabbro was intruded first as a mafic differentiate of the Oregon Dome/Snowy Mountain Dome magma, and was later intruded by the anorthositic gabbro. This later intrusion was concurrent with the emplacement of the Speculator Sheet and the Thirteenth Lake Dome. These data suggest that the contacts of anorthosites against country rock in the southern Adirondacks are igneous and not the product of sedimentation on an anorthositic basement. Textural and analytical evidence and graphical analysis suggest that the differing metamorphic mineral assemblages are controlled by variations in water fugacity. The development of orthopyroxene-plagio-clase coronas on some of the garnets is dependent on the iron contents of the garnets.

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
1981

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Beddoe, Theresa Anne

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/10919/54372
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/54372

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

Beddoe, Theresa Anne. Anorthositic sills of the southern Adirondack Mountains of New York state. masters thesis, Virginia Polytechnic Institute and State University, 1981. http://hdl.handle.net/10919/54372