A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica

Includes bibliographical references. The Sverdrupfjella Group in western Dronning Maud Land forms part of a 1200 Ma to 900 Ma orogenic belt which experienced a thermal overprint at around 500 Ma. Although the degree of tectonic reworking during this later event remains uncertain, evidence for late f...

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Bibliographic Details
Main Author: Johnstone, Warren Peter
Other Authors: Harris, Chris
Format: Master Thesis
Language:English
Published: University of Cape Town 2001
Subjects:
Online Access:http://hdl.handle.net/11427/9706
https://open.uct.ac.za/bitstream/11427/9706/1/thesis_sci_2001_johnstone_wp%20%281%29.pdf
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spelling ftunivcapetownir:oai:localhost:11427/9706 2023-05-15T13:32:18+02:00 A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica Johnstone, Warren Peter Harris, Chris 2001 application/pdf http://hdl.handle.net/11427/9706 https://open.uct.ac.za/bitstream/11427/9706/1/thesis_sci_2001_johnstone_wp%20%281%29.pdf eng eng University of Cape Town Faculty of Science Department of Geological Sciences http://hdl.handle.net/11427/9706 https://open.uct.ac.za/bitstream/11427/9706/1/thesis_sci_2001_johnstone_wp%20%281%29.pdf Earth Sciences Master Thesis Masters MSc 2001 ftunivcapetownir 2022-09-13T05:55:43Z Includes bibliographical references. The Sverdrupfjella Group in western Dronning Maud Land forms part of a 1200 Ma to 900 Ma orogenic belt which experienced a thermal overprint at around 500 Ma. Although the degree of tectonic reworking during this later event remains uncertain, evidence for late fluid alteration is widespread. In this study, the high-grade metamorphic rocks which make up the Sverdrupfjella Group were sampled in the central Kirwanveggen area. The stable isotope and whole-rock composition of these rocks have been determined, in order to test whether zones of intense fluid-rock interaction can be used as evidence for Pan African overprinting of Grenvillian orogenesis in western Dronning Maud Land. Master Thesis Antarc* Antarctica Dronning Maud Land East Antarctica University of Cape Town: OpenUCT Dronning Maud Land East Antarctica Kirwanveggen ENVELOPE(-3.500,-3.500,-73.500,-73.500) Sverdrupfjella ENVELOPE(0.583,0.583,-72.700,-72.700)
institution Open Polar
collection University of Cape Town: OpenUCT
op_collection_id ftunivcapetownir
language English
topic Earth Sciences
spellingShingle Earth Sciences
Johnstone, Warren Peter
A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica
topic_facet Earth Sciences
description Includes bibliographical references. The Sverdrupfjella Group in western Dronning Maud Land forms part of a 1200 Ma to 900 Ma orogenic belt which experienced a thermal overprint at around 500 Ma. Although the degree of tectonic reworking during this later event remains uncertain, evidence for late fluid alteration is widespread. In this study, the high-grade metamorphic rocks which make up the Sverdrupfjella Group were sampled in the central Kirwanveggen area. The stable isotope and whole-rock composition of these rocks have been determined, in order to test whether zones of intense fluid-rock interaction can be used as evidence for Pan African overprinting of Grenvillian orogenesis in western Dronning Maud Land.
author2 Harris, Chris
format Master Thesis
author Johnstone, Warren Peter
author_facet Johnstone, Warren Peter
author_sort Johnstone, Warren Peter
title A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica
title_short A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica
title_full A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica
title_fullStr A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica
title_full_unstemmed A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica
title_sort stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, east antarctica
publisher University of Cape Town
publishDate 2001
url http://hdl.handle.net/11427/9706
https://open.uct.ac.za/bitstream/11427/9706/1/thesis_sci_2001_johnstone_wp%20%281%29.pdf
long_lat ENVELOPE(-3.500,-3.500,-73.500,-73.500)
ENVELOPE(0.583,0.583,-72.700,-72.700)
geographic Dronning Maud Land
East Antarctica
Kirwanveggen
Sverdrupfjella
geographic_facet Dronning Maud Land
East Antarctica
Kirwanveggen
Sverdrupfjella
genre Antarc*
Antarctica
Dronning Maud Land
East Antarctica
genre_facet Antarc*
Antarctica
Dronning Maud Land
East Antarctica
op_relation http://hdl.handle.net/11427/9706
https://open.uct.ac.za/bitstream/11427/9706/1/thesis_sci_2001_johnstone_wp%20%281%29.pdf
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