The petrology of the alkali intrusive rocks from the Erongo volcanic complex select="/dri:document/dri:meta/dri:pageMeta/dri:metadata[@element='title']/node()"/>

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dc.contributor.advisor Marsh JS en_US
dc.contributor.advisor Pirajno F en_US
dc.contributor.author Patel S en_US
dc.date.accessioned 2013-07-02T14:10:43Z
dc.date.available 2013-07-02T14:10:43Z
dc.date.issued 1998 en_US
dc.identifier.uri http://hdl.handle.net/11070.1/4453
dc.description.abstract Abstract provided by author: en_US
dc.description.abstract In comparison with primordial mantle composition these alkali intrusive rocks are generally enriched in highly incompatible elements such as Nb and P, with low values for K and Ba en_US
dc.description.abstract Geochemical features observed show that the basanites are distinct from the other rock types. Their primitive character is reflected by high contents of Nb, Zr, Ba, Sr, and Y, and relatively low contents of Rb, Th and Pb. The tephrite-phonotephrite-tephriphonolite-phonolites represent products of a number of lineages related by similar parent compositions. Fractional crystallisation results in increasing SiO2, K2O, Al2O3 and Na2O, Rb, Th and Pb, but decreasing total iron, MgO, CaO, Ti02, Co, Cu, V, Ba and Sr en_US
dc.format.extent 34 p en_US
dc.language.iso eng en_US
dc.subject Geology en_US
dc.subject Petrology en_US
dc.title The petrology of the alkali intrusive rocks from the Erongo volcanic complex en_US
dc.type thesis en_US
dc.identifier.isis F004-199299999999999 en_US
dc.description.degree Grahamstown en_US
dc.description.degree South Africa en_US
dc.description.degree Rhodes University en_US
dc.description.degree B Sc Hons Geology en_US
dc.masterFileNumber 2769 en_US


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