Alkaline igneous rocks of the coastal belt, south of Luderitz, South West Africa : a petrological study
dc.contributor.author | Marsh, Julian Saville | en_ZA |
dc.date.accessioned | 2016-03-14T07:14:16Z | |
dc.date.available | 2016-03-14T07:14:16Z | |
dc.date.issued | 1973 | en_ZA |
dc.description.abstract | The Luderitz Alkaline Province, as it is at present known, comprises the subvolcanic central complexes of Drachenberg, Pomona, and Granitberg. An attendant dyke swarm strikes NE-SW and crops out between the latitudes of 27°00' and 27°30' S. Stratigraphic indications (now confirmed by a K/Ar age from Granitberg) are that the Luderitz Province is early-Cretaceous in age and therefore older than the Klinghardt phonolites (Eocene) as well as the smaller melilitite and nephelinite intrusions. Granitberg is a circular foyaite complex, in the centre of which is preserved a large fragment of sedimentary rocks that originally formed the roof of the intrusion. The foyaites have been emplaced into the feldspathic sandstones and dolomites of the Bogenfels Formation, and three major intrusive phases can be recognised. The first phase produced chilled nepheline syenites beneath the roof of the intrusion. These chilled rocks grade downwards into coarse-grained foyaites. The second phase was the emplacement of the Inner Foyaite which crystallized as a cylindrically zoned plug, capped by a zone of layered, laminated, and xenolithrich foyaites. The third phase was the emplacement of the Outer Foyaite, into which the Roof Zone and the Inner Foyaite foundered. The Outer Foyaite is zoned with a miaskitic core, and an agpaitic outer zone. | en_ZA |
dc.identifier.apacitation | Marsh, J. S. (1973). <i>Alkaline igneous rocks of the coastal belt, south of Luderitz, South West Africa : a petrological study</i>. (Thesis). University of Cape Town ,Faculty of Science ,Department of Geological Sciences. Retrieved from http://hdl.handle.net/11427/17697 | en_ZA |
dc.identifier.chicagocitation | Marsh, Julian Saville. <i>"Alkaline igneous rocks of the coastal belt, south of Luderitz, South West Africa : a petrological study."</i> Thesis., University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 1973. http://hdl.handle.net/11427/17697 | en_ZA |
dc.identifier.citation | Marsh, J. 1973. Alkaline igneous rocks of the coastal belt, south of Luderitz, South West Africa : a petrological study. University of Cape Town. | en_ZA |
dc.identifier.ris | TY - Thesis / Dissertation AU - Marsh, Julian Saville AB - The Luderitz Alkaline Province, as it is at present known, comprises the subvolcanic central complexes of Drachenberg, Pomona, and Granitberg. An attendant dyke swarm strikes NE-SW and crops out between the latitudes of 27°00' and 27°30' S. Stratigraphic indications (now confirmed by a K/Ar age from Granitberg) are that the Luderitz Province is early-Cretaceous in age and therefore older than the Klinghardt phonolites (Eocene) as well as the smaller melilitite and nephelinite intrusions. Granitberg is a circular foyaite complex, in the centre of which is preserved a large fragment of sedimentary rocks that originally formed the roof of the intrusion. The foyaites have been emplaced into the feldspathic sandstones and dolomites of the Bogenfels Formation, and three major intrusive phases can be recognised. The first phase produced chilled nepheline syenites beneath the roof of the intrusion. These chilled rocks grade downwards into coarse-grained foyaites. The second phase was the emplacement of the Inner Foyaite which crystallized as a cylindrically zoned plug, capped by a zone of layered, laminated, and xenolithrich foyaites. The third phase was the emplacement of the Outer Foyaite, into which the Roof Zone and the Inner Foyaite foundered. The Outer Foyaite is zoned with a miaskitic core, and an agpaitic outer zone. DA - 1973 DB - OpenUCT DP - University of Cape Town LK - https://open.uct.ac.za PB - University of Cape Town PY - 1973 T1 - Alkaline igneous rocks of the coastal belt, south of Luderitz, South West Africa : a petrological study TI - Alkaline igneous rocks of the coastal belt, south of Luderitz, South West Africa : a petrological study UR - http://hdl.handle.net/11427/17697 ER - | en_ZA |
dc.identifier.uri | http://hdl.handle.net/11427/17697 | |
dc.identifier.vancouvercitation | Marsh JS. Alkaline igneous rocks of the coastal belt, south of Luderitz, South West Africa : a petrological study. [Thesis]. University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 1973 [cited yyyy month dd]. Available from: http://hdl.handle.net/11427/17697 | en_ZA |
dc.language.iso | eng | en_ZA |
dc.publisher.department | Department of Geological Sciences | en_ZA |
dc.publisher.faculty | Faculty of Science | en_ZA |
dc.publisher.institution | University of Cape Town | |
dc.subject.other | Geology | en_ZA |
dc.subject.other | Petrology | en_ZA |
dc.title | Alkaline igneous rocks of the coastal belt, south of Luderitz, South West Africa : a petrological study | en_ZA |
dc.type | Doctoral Thesis | |
dc.type.qualificationlevel | Doctoral | |
dc.type.qualificationname | PhD | en_ZA |
uct.type.filetype | Text | |
uct.type.filetype | Image | |
uct.type.publication | Research | en_ZA |
uct.type.resource | Thesis | en_ZA |
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