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A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica
Includes bibliographical references.
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| Main Author: | |
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| Other Authors: | |
| Format: | Thesis |
| Language: | English |
| Published: |
Department of Geological Sciences
2014
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| _version_ | 1867613445344460800 |
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| access_status_str | Open Access |
| author | Johnstone, Warren Peter |
| author2 | Harris, Chris |
| author_browse | Harris, Chris Johnstone, Warren Peter |
| author_facet | Harris, Chris Johnstone, Warren Peter |
| author_sort | Johnstone, Warren Peter |
| collection | Thesis |
| description | Includes bibliographical references. |
| format | Thesis |
| id | oai:open.uct.ac.za:11427/9706 |
| institution | University of Cape Town (South Africa) |
| language | eng |
| last_indexed | 2026-06-10T12:36:15.800Z |
| license_str | Not specified — see source repository |
| provenance_str_mv | Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository |
| publishDate | 2014 |
| publishDateRange | 2014 |
| publishDateSort | 2014 |
| publisher | Department of Geological Sciences |
| publisherStr | Department of Geological Sciences |
| record_format | dspace |
| source_str | UCTD — University of Cape Town Open Access Repository |
| spelling | oai:open.uct.ac.za:11427/9706 A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica Johnstone, Warren Peter Harris, Chris Earth Sciences 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. 2014-11-18T17:03:51Z 2014-11-18T17:03:51Z 2001 Master Thesis Masters MSc http://hdl.handle.net/11427/9706 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town |
| spellingShingle | Earth Sciences Johnstone, Warren Peter A stable isotope investigation into fluid-rock interaction during regional metamorphism in western dronning maud land, East Antarctica |
| thesis_degree_str | Master's |
| title | 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_short | 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 |
| topic | Earth Sciences |
| url | http://hdl.handle.net/11427/9706 |
| work_keys_str_mv | AT johnstonewarrenpeter astableisotopeinvestigationintofluidrockinteractionduringregionalmetamorphisminwesterndronningmaudlandeastantarctica AT johnstonewarrenpeter stableisotopeinvestigationintofluidrockinteractionduringregionalmetamorphisminwesterndronningmaudlandeastantarctica |