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Petrogenesis of hybrid porphyry pipes and evolution of alkaline magmas in the Kanabeam Igneous Complex, Southern Namibia

Includes bibliography.

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Bibliographic Details
Main Author: Dunn, Natalie Kirsty
Other Authors: Reid, David
Format: Thesis
Language:English
Published: Department of Geological Sciences 2014
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access_status_str Open Access
author Dunn, Natalie Kirsty
author2 Reid, David
author_browse Dunn, Natalie Kirsty
Reid, David
author_facet Reid, David
Dunn, Natalie Kirsty
author_sort Dunn, Natalie Kirsty
collection Thesis
description Includes bibliography.
format Thesis
id oai:open.uct.ac.za:11427/4195
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:32:38.580Z
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:11427/4195 Petrogenesis of hybrid porphyry pipes and evolution of alkaline magmas in the Kanabeam Igneous Complex, Southern Namibia Dunn, Natalie Kirsty Reid, David Geological Sciences Includes bibliography. The linear Kuboos Bremen Igneous Province (KBIP) stretches 270km from the South African Atlantic coast north-eastwards into southern Namibia, and was emplaced at approximately 500Ma. One central complex within the KBIP is the Kanabeam Igneous Complex (KIC) where practically all the rock types found in the province are represented and include nepheline syenites, quartz syenites as well as granites. In addition to these plutonic phases a number of late stage, xenolith rich porphyry pipes were emplaced, exploiting contact zones between earlier plutons. Xenolith types include gabbro possibly derived from unexposed deeper parts of the KIC, syenites (more proximal components of the KIC), trachytes from an inferred overlying volcanic edifice, basement granites, gneisses and metasediments as well as Nama Group sediments. Petrographicl examination in the porphyries has releaved that there are numerous minerals out of textual equilibrium, including olivine, pyroxene and plagioclase. Other minerals such as biotite, amphibole and alkali feldspar appear more stable. 2014-07-30T17:26:10Z 2014-07-30T17:26:10Z 2001 Master Thesis Masters MSc http://hdl.handle.net/11427/4195 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Geological Sciences
Dunn, Natalie Kirsty
Petrogenesis of hybrid porphyry pipes and evolution of alkaline magmas in the Kanabeam Igneous Complex, Southern Namibia
thesis_degree_str Master's
title Petrogenesis of hybrid porphyry pipes and evolution of alkaline magmas in the Kanabeam Igneous Complex, Southern Namibia
title_full Petrogenesis of hybrid porphyry pipes and evolution of alkaline magmas in the Kanabeam Igneous Complex, Southern Namibia
title_fullStr Petrogenesis of hybrid porphyry pipes and evolution of alkaline magmas in the Kanabeam Igneous Complex, Southern Namibia
title_full_unstemmed Petrogenesis of hybrid porphyry pipes and evolution of alkaline magmas in the Kanabeam Igneous Complex, Southern Namibia
title_short Petrogenesis of hybrid porphyry pipes and evolution of alkaline magmas in the Kanabeam Igneous Complex, Southern Namibia
title_sort petrogenesis of hybrid porphyry pipes and evolution of alkaline magmas in the kanabeam igneous complex southern namibia
topic Geological Sciences
url http://hdl.handle.net/11427/4195
work_keys_str_mv AT dunnnataliekirsty petrogenesisofhybridporphyrypipesandevolutionofalkalinemagmasinthekanabeamigneouscomplexsouthernnamibia