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James Cook University

Reconciling the structural and metamorphic record of orogeny in central western New Hampshire through microstructure and garnet isopleth thermobarometry

Abstract

dc:description.abstract

This thesis consists of four sections, each a stand-alone body of work intended for publication in international journals. The sections are ordered such that they progress in a logical fashion; the first two sections form an introduction to the new analytical techniques developed and utilised within this thesis, the remaining two sections present data and geological interpretations derived from the application of these techniques. Volume 1 contains the text and reference list, whilst Volume 2 contains the figures and appendices. Section A describes the technique of garnet isopleth thermobarometry, and outlines methods for analysing the relative contributions of the sources of error inherent to this technique. Additionally, some insights into the significance of common compositional variations within garnet are provided and discussed. Section B describes a method for calculating the changes in composition of the chemical system from which garnet is growing that are caused by crystal fractionation of garnet. This section has been published in The Journal of Metamorphic Geology (Evans, 2004), and is presented here unchanged. Section C utilises the methods described in the first two sections to determine a metamorphic history for the Garnet Hill and Salmon Hole Brook synclines of central western New Hampshire, USA. The thermal regime of the region during metamorphism was found to be characterised by localised, transient thermal heterogeneities. Two distinct episodes of metasomatism were also defined. Section D utilises the methods described in the first two sections to test a previously defined relative timing scheme for porphyroblast growth that was based on Foliation Intersection Axes preserved within porphyroblast (FIA). Additionally, a tectonic model for central western New Hampshire is presented that explains several key geological features of the region that contradict many of the existing tectonic models.

Degree

thesis:*
Name dc:type.qualificationname
phd
Level dc:type.qualificationlevel
doctoral
Grantor dc:publisher.institution
James Cook University
Year dc:date.issued
2004

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Evans, Thomas Philip

Rights

Language dc:language
en

Chain of custody

source
Harvested from
James Cook University
Base URL
researchonline.jcu.edu.au/cgi/oai2
Last updated
2026-08-21
Source record
OAI-PMH GetRecord
related terms
citation

Evans, Thomas Philip. Reconciling the structural and metamorphic record of orogeny in central western New Hampshire through microstructure and garnet isopleth thermobarometry. doctoral thesis, James Cook University, 2004.