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A metamorphic and geochemical study of mafic rocks across the Pencksökket-Jutulstraumen Discontinuity, western Dronning Maud Land, East Antarctica

Includes bibliographical references (leaves 89-102).

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Bibliographic Details
Main Author: Grosch, Eugene Gerald
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 Grosch, Eugene Gerald
author2 Frimmel, Hartwig E
author_browse Frimmel, Hartwig E
Grosch, Eugene Gerald
author_facet Frimmel, Hartwig E
Grosch, Eugene Gerald
author_sort Grosch, Eugene Gerald
collection Thesis
description Includes bibliographical references (leaves 89-102).
format Thesis
id oai:open.uct.ac.za:11427/4199
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:34:08.683Z
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:11427/4199 A metamorphic and geochemical study of mafic rocks across the Pencksökket-Jutulstraumen Discontinuity, western Dronning Maud Land, East Antarctica Grosch, Eugene Gerald Frimmel, Hartwig E Geological Science Includes bibliographical references (leaves 89-102). A petrological and metamorphic comparison of Mesoproterozoic metabasic rocks on the easern margin of the Archaean Grunehogna Craton and the adjacent Maud Belt in western Dronning Maud Land, East Antarctica, revealed a difference in peak metamorphic conditions from T = ~275° to 730°C and P=2 to 10.7 kbar over a distance of only 30 km across a major glacial valley. The lower grade constraints were derived from average P-T calculations using THER-MOCALC and thermodynamic modeling of phase equilibria together with chlorite geothermometry. The high-grade P-T constraint for the westernmost part of the Maud Belt closest to the glacier, derived from hornblende-plagioclase thermometry and geobarometric calculations with a garnet amphibolite assemblage, is very similar to that reported for the eastern Maud Belt and, therefore, does not support the concept of a westward decreasing metamorphic field gradient as previously proposed. In conjunction with a recent geochronological study on the eastern Maud Belt, this study suggests that the inferred sub-glacial boundary between the Grunehogna Craton and the Maud Belt, known as the Pencksökket-Jutulstraumen Discontinuity, may represent a major thrust that developed during Pan-African orogenesis (possibly as the continuation of the East African Mozambique Belt into East Antarctica) prior to extension and its development as a normal listric fault or succession of fault slices during the Mesozoic break-up of Gondwana. 2014-07-30T17:26:17Z 2014-07-30T17:26:17Z 2005 Master Thesis Masters MSc http://hdl.handle.net/11427/4199 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Geological Science
Grosch, Eugene Gerald
A metamorphic and geochemical study of mafic rocks across the Pencksökket-Jutulstraumen Discontinuity, western Dronning Maud Land, East Antarctica
thesis_degree_str Master's
title A metamorphic and geochemical study of mafic rocks across the Pencksökket-Jutulstraumen Discontinuity, western Dronning Maud Land, East Antarctica
title_full A metamorphic and geochemical study of mafic rocks across the Pencksökket-Jutulstraumen Discontinuity, western Dronning Maud Land, East Antarctica
title_fullStr A metamorphic and geochemical study of mafic rocks across the Pencksökket-Jutulstraumen Discontinuity, western Dronning Maud Land, East Antarctica
title_full_unstemmed A metamorphic and geochemical study of mafic rocks across the Pencksökket-Jutulstraumen Discontinuity, western Dronning Maud Land, East Antarctica
title_short A metamorphic and geochemical study of mafic rocks across the Pencksökket-Jutulstraumen Discontinuity, western Dronning Maud Land, East Antarctica
title_sort metamorphic and geochemical study of mafic rocks across the pencksokket jutulstraumen discontinuity western dronning maud land east antarctica
topic Geological Science
url http://hdl.handle.net/11427/4199
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AT groscheugenegerald metamorphicandgeochemicalstudyofmaficrocksacrossthepencksokketjutulstraumendiscontinuitywesterndronningmaudlandeastantarctica