- Title
- The extrusive and intrusive basaltic rocks of the Molteno-Jamestown area
- Creator
- Mitchell, Andrew Alexander
- ThesisAdvisor
- Eales, H V
- ThesisAdvisor
- Marsh, J S
- Subject
- Basalt -- South Africa -- Cape of Good Hope
- Date
- 1980
- Type
- Thesis
- Type
- Masters
- Type
- MSc
- Identifier
- vital:4900
- Identifier
- http://hdl.handle.net/10962/d1001559
- Description
- The Karoo basalt outliers between Molteno and Jamestown in the north-eastern Cape Province are associated with two central volcanic vent complexes, referred to in the text as the Brosterlea and the Modderfontein complexes. The basalts, particularly those associated with the Brosterlea complex, show geochemical variations throughout the sequence, a factor which has facilitated the subdivision of the Brosterlea basalts into a series of discrete units, each having its own chemical characteristics. Most of the basalt units at Brosterlea can be correlated with units identified in the Barkly East basalt suite. As is the case around Barkly East, the Brosterlea basalt units cannot be related to one another by any simple crystal fractionation or partial melting process, and the most feasible alternative explanation lies in the existence of inhomogeneities in the upper mantle at the time of generation of the magmas. New electron microprobe data are presented for the silicate phases in the Karoo basalts. Analyses of augites from a limited number of slides indicate that pyroxenes from different basalt units define different trends on the Ca - Mg - Fe triangular diagram. The plagioclases in the Brosterlea basalts are fairly Ca-rich (average 70% An), and the K-content of the plagioclases is shown to vary with the K-content of the parent basalt. A comparison of the Karoo Central Province with the younger Columbia River and Deccan Trap Provinces shows many similarities in the evolutionary history of the three provinces. The Karoo Province, however, is distinct from the other two provinces in some aspects of the geochemistry. Broadly speaking, the Karoo basalts are depleted in the incompatible elements relative to the Columbia River and Deccan basalts, and often enriched in the transition metals, most specifically Cr
- Format
- 203 leaves, pdf
- Publisher
- Rhodes University, Faculty of Science, Geology
- Language
- English
- Rights
- Mitchell, Andrew Alexander
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