- Title
- Mineralogy and petrology of the Townlands iron-rich ultramafic pegmatite
- Creator
- Phillips, David
- ThesisAdvisor
- Reynolds, I. M.
- Subject
- Ultrabasic rocks -- South African -- Rustenburg
- Subject
- Platinum ores -- South Africa -- Rustenburg
- Subject
- Pegmatites -- South Africa -- Rustenburg
- Subject
- Mines and mineral resources -- South Africa -- Rustenburg
- Date
- 1985
- Date
- 2013-09-09
- Type
- Thesis
- Type
- Masters
- Type
- MSc
- Identifier
- vital:5040
- Identifier
- http://hdl.handle.net/10962/d1007617
- Identifier
- Ultrabasic rocks -- South African -- Rustenburg
- Identifier
- Platinum ores -- South Africa -- Rustenburg
- Identifier
- Pegmatites -- South Africa -- Rustenburg
- Identifier
- Mines and mineral resources -- South Africa -- Rustenburg
- Description
- The Townlands iron-rich ultramafic pegmatite is a relatively large pipelike body situated in the western corner of Rustenburg Section, Rustenburg Platinum Mines. It is characterised by a strong negative magnetic signature and transgresses the noritic layered sequence of the upper critical zone of the Bushveld Complex. The layered rocks are downwarped in the vicinity of the pipe and are in sharp contact with the pegmatitic material. The pegmatite varies in composition between dunite and wehrlite, with the marginal zones being more wehrlitic in composition. Olivine (Fo₃₀ - Fo₅₂) and clinopyroxene (Wo₄₅En₃₀Fs₂₅ - Wo₄₅En₃₇Fs₁₈) are the dominant constituents and accessory phases include ilmenite, Ti -magnetite, apatite, amphiboles, chlorite-group minerals, biotite, ilvaite and a host of unusual ore minerals. The Fe-Ti oxides exhibit exsolution textures typically found in slowly cooled igneous rocks and temperatures of formati on are consi dered to be in excess of 800°C. The UG2 chromitite leader layers intersected by borehole TLP.l are enriched in Fe and Ti and exhibit compositions intermediate between chromite and Ti-magnetite. The ore mineral assemblage includes a primary sulphide assemblage consisting of troilite, chalcopyrite, cubanite and pentlandite, and an array of unusual phases formed by late-stage secondary processes. The unusual sulphides mooihoekite and haycockite, that occur in certain parts of the pegmatite, are considered to have formed by partial replacement of the primary assemblage and a possible paragenetic sequence is discussed. Mineral compositions and whole rock geochemical data are consistent with an origin for the pegmatite by crystallization from a fractionated melt. It is suggested that intercumulus fluids, trapped during the crystallization of the noritic layered sequence, accumulated in an area of structural weakness, in response to an increasing overburden pressure and/or tectonic activity. Evidence is also presented that indicates that the Townlands pegmatite may consist of at least two separate, but adjoining pegmatite bodies.
- Description
- KMBT_363
- Description
- Adobe Acrobat 9.54 Paper Capture Plug-in
- Format
- 188 p., pdf
- Publisher
- Rhodes University, Faculty of Science, Geology
- Language
- English
- Rights
- Phillips, David
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