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High-grade metamorphism and migmatizaof the Namaqua metamorphic complex around Aus in the Southern Namib Desert, South West Africa

Bibliography : pages 261-277.

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Main Author: Jackson, MPA
Other Authors: De Villiers, John
Format: Thesis
Language:English
Published: Department of Geological Sciences 2016
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access_status_str Open Access
author Jackson, MPA
author2 De Villiers, John
author_browse De Villiers, John
Jackson, MPA
author_facet De Villiers, John
Jackson, MPA
author_sort Jackson, MPA
collection Thesis
description Bibliography : pages 261-277.
format Thesis
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institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:33:08.525Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2016
publishDateRange 2016
publishDateSort 2016
publisher Department of Geological Sciences
publisherStr Department of Geological Sciences
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source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/16621 High-grade metamorphism and migmatizaof the Namaqua metamorphic complex around Aus in the Southern Namib Desert, South West Africa Jackson, MPA De Villiers, John Kroner, A Geological Sciences Bibliography : pages 261-277. Rocks of the Namaqua Metamorphic Complex are exposed in an area of 10 000 km² in the northwestern part of the Namaqua Mobile Belt east of Liideritz. The Garub sequence represents the oldest rocks in the Aus area and comprises a diverse group of layered rocks of mainly semi-pelitic, pelitic, mafic, calcareous and quartzose composition. These rocks have been metamorphosed to form marbles, calcitic gneisses, metaquartzites, biotite schists, sillimanitecordierite garnet gneisses, amphibolites and granolites with minor amounts of iron formation and magnesian rocks. The principal metasediments are concentrated in west-trending zones. A central zone of calcareous rocks broadens westwards and contains the largest known bodies of carbonate rocks in the Namaqua Metamorphic Complex. The calcareous zone is bounded in the north by a narrow beit of quartzose rocks and in the south, by a broad zone of aluminous rocks. Gradational rock types between these zones are compatible with original sedimentary lithofacies changes. Layered biotite gneiss of psammitic composition has been interfolded with units of the Garub sequence. Both these rock units are present as inclusions within a tonalitic augen gneiss. 2016-02-01T09:58:41Z 2016-02-01T09:58:41Z 1976 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/16621 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Geological Sciences
Jackson, MPA
High-grade metamorphism and migmatizaof the Namaqua metamorphic complex around Aus in the Southern Namib Desert, South West Africa
thesis_degree_str Doctoral
title High-grade metamorphism and migmatizaof the Namaqua metamorphic complex around Aus in the Southern Namib Desert, South West Africa
title_full High-grade metamorphism and migmatizaof the Namaqua metamorphic complex around Aus in the Southern Namib Desert, South West Africa
title_fullStr High-grade metamorphism and migmatizaof the Namaqua metamorphic complex around Aus in the Southern Namib Desert, South West Africa
title_full_unstemmed High-grade metamorphism and migmatizaof the Namaqua metamorphic complex around Aus in the Southern Namib Desert, South West Africa
title_short High-grade metamorphism and migmatizaof the Namaqua metamorphic complex around Aus in the Southern Namib Desert, South West Africa
title_sort high grade metamorphism and migmatizaof the namaqua metamorphic complex around aus in the southern namib desert south west africa
topic Geological Sciences
url http://hdl.handle.net/11427/16621
work_keys_str_mv AT jacksonmpa highgrademetamorphismandmigmatizaofthenamaquametamorphiccomplexaroundausinthesouthernnamibdesertsouthwestafrica