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Tectono-thermal evolution of Gjelsvikfjella, Western Dronning Maud Land, Antarctica

Includes bibliographical references (leaves 99-117).

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Bibliographic Details
Main Author: Bisnath, Avinash
Other Authors: Frimmel, Hartwig E
Format: Thesis
Language:English
Published: Department of Geological Sciences 2014
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access_status_str Open Access
author Bisnath, Avinash
author2 Frimmel, Hartwig E
author_browse Bisnath, Avinash
Frimmel, Hartwig E
author_facet Frimmel, Hartwig E
Bisnath, Avinash
author_sort Bisnath, Avinash
collection Thesis
description Includes bibliographical references (leaves 99-117).
format Thesis
id oai:open.uct.ac.za:11427/4188
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:31:38.662Z
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
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spelling oai:open.uct.ac.za:11427/4188 Tectono-thermal evolution of Gjelsvikfjella, Western Dronning Maud Land, Antarctica Bisnath, Avinash Frimmel, Hartwig E Geological Sciences Includes bibliographical references (leaves 99-117). East Antarctica is dominated by the East Antarctic Craton, which consists of fragments of Archaean continental crust surrounded by polydeformed orogenic belts (e.g. Maud Belt). The Maud Belt in Dronning Maud Land preserves a high-grade polyphase tectono-thermal history. This belt has traditionally been interpreted as a Mesoproterozoic-age (1.3-0.9 Ga) mobile belt that was later affected by thermal overprint associated with little or no deformation during the Neoproterozoic (0.6-0.5 Ga). Therefore the Maud Belt has been used as a piercing point in Mesoproterozoic supercontinent reconstruction. However, with the growing number of geochronological data pointing to major structural reworking and not just a thermal overprint of the Mesoproterozoic crust during the Pan-African orogeny thereby challenging early models of Mesoproterozoic supercontinent reconstruction. Areas east and west of Gjelsvikfjella record major Pan-African reworking. Thus the outcrops of Gjelsvikfjella provide the linkage between the two areas. Yet, so far little data has been available for this crucial sector. Therefore, detailed fieldwork in the Gjelsvikfjella coupled with petrographic, geochemical and geochronogical data obtained from carefully selected samples reveal a complex tectono-thermal history for this part of the Maud Belt. The SHRIMP U-Pb zircon data obtained make it possible to differentiate between a series of magmatic and metamorphic events. The oldest event recorded is the formation of an extensive, 1140-1130 Ma, volcanic arc. This was followed by 1104 ± 8 Ma granitoids that might represent, together with so far undated mafic dykes part of a decompression melting-related bimodal suite. Only very few relics of late Mesoproterozoic granulite-facies metamorphism is constrained in 1070 Ma strain-protected domains. 2014-07-30T17:25:22Z 2014-07-30T17:25:22Z 2005 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/4188 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Geological Sciences
Bisnath, Avinash
Tectono-thermal evolution of Gjelsvikfjella, Western Dronning Maud Land, Antarctica
thesis_degree_str Doctoral
title Tectono-thermal evolution of Gjelsvikfjella, Western Dronning Maud Land, Antarctica
title_full Tectono-thermal evolution of Gjelsvikfjella, Western Dronning Maud Land, Antarctica
title_fullStr Tectono-thermal evolution of Gjelsvikfjella, Western Dronning Maud Land, Antarctica
title_full_unstemmed Tectono-thermal evolution of Gjelsvikfjella, Western Dronning Maud Land, Antarctica
title_short Tectono-thermal evolution of Gjelsvikfjella, Western Dronning Maud Land, Antarctica
title_sort tectono thermal evolution of gjelsvikfjella western dronning maud land antarctica
topic Geological Sciences
url http://hdl.handle.net/11427/4188
work_keys_str_mv AT bisnathavinash tectonothermalevolutionofgjelsvikfjellawesterndronningmaudlandantarctica