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Mineralised Pegmatites of the Damara Belt, Namibia: Fluid Inclusion and Geochemical Characteristics with Implications for Post- Collisional Mineralisation
Mineralised Pegmatites of the Damara Belt, Namibia: Fluid inclusion and geochemical characteristics with implications for post- collisional mineralisation Luisa Ashworth A dissertation submitted to the Fa culty of Science, University of the Witwatersrand, Johannesburg, in fulfilment of the requirements for the degree of Doctor of Philosophy. Johannesburg, 2014 DECLARATION I declare that this thesis is my own, unaided work. It is being submitted for the degree of Doctor of Philosophy at the University of the Witwatersrand, Johannesburg. It has not been submitted before for any degree or examination in any other university. _______________________ Luisa Ashworth 20 of March 2014 i ABSTRACT Namibia is renowned for its abundant mineral resources, a large proportion of which are hosted in the metasedimentary lithologies of the Damara Belt, the northeast-trending inland branch of the Neoproterozoic Pan-African Damara Orogen. Deposit types include late- to post-tectonic (~ 523 – 506 Ma) LCT (Li-Be, Sn-, and miarolitic gem-tourmaline- bearing) pegmatites, and uraniferous pegmatitic sheeted leucogranites (SLGs), which have an NYF affinity. Fluid inclusion studies reveal that although mineralization differs between the different types of pegmatites located at different geographic locations, and by extension, different stratigraphic levels, the fluid inclusion assemblages present in these pegmatites are similar; thus different types of pegmatites are indistinguishable from each other based on their fluid inclusion assemblages. Thorough fluid inclusion petrography indicated that although fluid inclusions are abundant in the pegmatites, no primary fluid inclusions could be identified, and rather those studied are pseudosecondary and secondary. Fluid inclusions are aqueo-carbonic (± NaCl), carbonic, and aqueous. It is proposed that all of the pegmatites studied share a similar late-stage evolution, with fluids becoming less carbonic and less saline with the progression of crystallisation. -
1 Revision 2 1 K-Bentonites
1 Revision 2 2 K-Bentonites: A Review 3 Warren D. Huff 4 Department of Geology, University of Cincinnati, Cincinnati, OH 45221 USA 5 Email: [email protected] 6 Keywords: K-bentonite, bentonite, tephra, explosive volcanism, volcanic ash 7 Abstract 8 Pyroclastic material in the form of altered volcanic ash or tephra has been reported and described 9 from one or more stratigraphic units from the Proterozoic to the Tertiary. This altered tephra, 10 variously called bentonite or K-bentonite or tonstein depending on the degree of alteration and 11 chemical composition, is often linked to large explosive volcanic eruptions that have occurred 12 repeatedly in the past. K-bentonite and bentonite layers are the key components of a larger group of 13 altered tephras that are useful for stratigraphic correlation and for interpreting the geodynamic 14 evolution of our planet. Bentonites generally form by diagenetic or hydrothermal alteration under 15 the influence of fluids with high Mg content and that leach alkali elements. Smectite composition is 16 partly controlled by parent rock chemistry. Studies have shown that K-bentonites often display 17 variations in layer charge and mixed-layer clay ratios and that these correlate with physical 18 properties and diagenetic history. The following is a review of known K-bentonite and related 19 occurrences of altered tephra throughout the time scale from Precambrian to Cenozoic. 20 Introduction 21 Volcanic eruptions are often, although by no means always, associated with a profuse output 22 of fine pyroclastic material, tephra. Tephra is a term used to describe all of the solid material 23 produced from a volcano during an eruption (Thorarinsson, 1944). -
South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
Palaeontological Impact Assessment May Be Significantly Enhanced Through Field Assessment by a Professional Palaeontologist
PALAEONTOLOGICAL SPECIALIST STUDY: COMBINED DESKTOP & FIELD-BASED ASSESSMENT Four proposed solar PV projects on Farm Visserspan No. 40 near Dealesville, Tokologo Local Municipality, Free State Province John E. Almond PhD (Cantab.) Natura Viva cc, PO Box 12410 Mill Street, Cape Town 8010, RSA [email protected] January 2020 EXECUTIVE SUMMARY Ventura Renewable Energy (Pty) Ltd is proposing to develop up to four solar PV facilities, each of up to 100 MW generation capacity, on the farm Visserspan No. 40, c. 10 km northwest of Dealesville and 68 km northwest of Bloemfontein, in the Tokologo Local Municipality, Free State Province. Substantial direct impacts on fresh, potentially-fossiliferous Tierberg Formation (Ecca Group, Karoo Supergroup) bedrocks during the construction phase of the proposed PV solar projects are considered unlikely. The mapped outcrop areas of the Tierberg Formation within the PV solar project areas are small while the mudocks here are likely to be weathered near-surface and mantled by thick superficial deposits such as calcrete. In this region, the near-surface Ecca Group bedrocks are very often extensively disrupted and veined by Quaternary calcrete as well as baked by dolerite intrusions, compromising their palaeontological sensitivity. Potentially fossiliferous Pleistocene alluvial or spring deposits were not encountered in the study area, while pan and associated dune sediments here lie largely – but not exclusively - outside the development footprint. The calcrete hardpans encountered within the study area are of low palaeontological sensitivity. The only fossil remains recorded during the field survey comprise a few small blocks of petrified fossil wood – reworked from Tierberg bedrocks - among surface gravels around the margins of a pan in the SE corner of Visserspan No. -
Geology of the Kranzberg Syncline and Emplacement Controls of the Usakos Pegmatite Field, Damara Belt, Central Namibia
GEOLOGY OF THE KRANZBERG SYNCLINE AND EMPLACEMENT CONTROLS OF THE USAKOS PEGMATITE FIELD, DAMARA BELT, CENTRAL NAMIBIA by Geoffrey J. Owen Thesis presented in fulfilment of the requirements for the degree Master of Science at the University of Stellenbosch Supervisor: Prof. Alex Kisters Faculty of Science Department of Earth Sciences March 2011 i DECLARATION By submitting this thesis electronically, I declare that the entirety of the work contained therein is my own, original work, that I am the sole author thereof (save to the extent explicitely otherwise stated), that reproduction and publication thereof by Stellenbosch University will not infringe any third party rights and that I have not previously in its entirety or in part submitted it for obtaining any qualification. Signature: Date: 15. February 2011 ii ABSTRACT The Central Zone (CZ) of the Damara belt in central Namibia is underlain by voluminous Pan-African granites and is host to numerous pegmatite occurrences, some of which have economic importance and have been mined extensively. This study discusses the occurrence, geometry, relative timing and emplacement mechanisms for the Usakos pegmatite field, located between the towns of Karibib and Usakos and within the core of the regional-scale Kranzberg syncline. Lithological mapping of the Kuiseb Formation in the core of the Kranzberg syncline identified four litho-units that form an up to 800 m thick succession of metaturbidites describing an overall coarsening upward trend. This coarsening upwards trend suggests sedimentation of the formation’s upper parts may have occurred during crustal convergence and basin closure between the Kalahari and Congo Cratons, rather than during continued spreading as previously thought. -
Xhariep Magisterial District
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The Role of Fossils in Interpreting the Development of the Karoo Basin
Palaeon!. afr., 33,41-54 (1997) THE ROLE OF FOSSILS IN INTERPRETING THE DEVELOPMENT OF THE KAROO BASIN by P. J. Hancox· & B. S. Rubidge2 IGeology Department, University of the Witwatersrand, Private Bag 3, Wits 2050, South Africa 2Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, Wits 2050, South Africa ABSTRACT The Permo-Carboniferous to Jurassic aged rocks oft1:J.e main Karoo Basin ofSouth Africa are world renowned for the wealth of synapsid reptile and early dinosaur fossils, which have allowed a ten-fold biostratigraphic subdivision ofthe Karoo Supergroup to be erected. The role offossils in interpreting the development of the Karoo Basin is not, however, restricted to biostratigraphic studies. Recent integrated sedimentological and palaeontological studies have helped in more precisely defming a number of problematical formational contacts within the Karoo Supergroup, as well as enhancing palaeoenvironmental reconstructions, and basin development models. KEYWORDS: Karoo Basin, Biostratigraphy, Palaeoenvironment, Basin Development. INTRODUCTION Invertebrate remains are important as indicators of The main Karoo Basin of South Africa preserves a facies genesis, including water temperature and salinity, retro-arc foreland basin fill (Cole 1992) deposited in as age indicators, and for their biostratigraphic potential. front of the actively rising Cape Fold Belt (CFB) in Fossil fish are relatively rare in the Karoo Supergroup, southwestern Gondwana. It is the deepest and but where present are useful indicators of gross stratigraphically most complete of several depositories palaeoenvironments (e.g. Keyser 1966) and also have of Permo-Carboniferous to Jurassic age in southern biostratigraphic potential (Jubb 1973; Bender et al. Africa and reflects changing depositional environments 1991). -
South Africa)
FREE STATE PROFILE (South Africa) Lochner Marais University of the Free State Bloemfontein, SA OECD Roundtable on Higher Education in Regional and City Development, 16 September 2010 [email protected] 1 Map 4.7: Areas with development potential in the Free State, 2006 Mining SASOLBURG Location PARYS DENEYSVILLE ORANJEVILLE VREDEFORT VILLIERS FREE STATE PROVINCIAL GOVERNMENT VILJOENSKROON KOPPIES CORNELIA HEILBRON FRANKFORT BOTHAVILLE Legend VREDE Towns EDENVILLE TWEELING Limited Combined Potential KROONSTAD Int PETRUS STEYN MEMEL ALLANRIDGE REITZ Below Average Combined Potential HOOPSTAD WESSELSBRON WARDEN ODENDAALSRUS Agric LINDLEY STEYNSRUST Above Average Combined Potential WELKOM HENNENMAN ARLINGTON VENTERSBURG HERTZOGVILLE VIRGINIA High Combined Potential BETHLEHEM Local municipality BULTFONTEIN HARRISMITH THEUNISSEN PAUL ROUX KESTELL SENEKAL PovertyLimited Combined Potential WINBURG ROSENDAL CLARENS PHUTHADITJHABA BOSHOF Below Average Combined Potential FOURIESBURG DEALESVILLE BRANDFORT MARQUARD nodeAbove Average Combined Potential SOUTPAN VERKEERDEVLEI FICKSBURG High Combined Potential CLOCOLAN EXCELSIOR JACOBSDAL PETRUSBURG BLOEMFONTEIN THABA NCHU LADYBRAND LOCALITY PLAN TWEESPRUIT Economic BOTSHABELO THABA PATSHOA KOFFIEFONTEIN OPPERMANSDORP Power HOBHOUSE DEWETSDORP REDDERSBURG EDENBURG WEPENER LUCKHOFF FAURESMITH houses JAGERSFONTEIN VAN STADENSRUST TROMPSBURG SMITHFIELD DEPARTMENT LOCAL GOVERNMENT & HOUSING PHILIPPOLIS SPRINGFONTEIN Arid SPATIAL PLANNING DIRECTORATE ZASTRON SPATIAL INFORMATION SERVICES ROUXVILLE BETHULIE -
Revealing the Beattie Magnetic Anomaly and the Anatomy Of
11th SAGA Biennial Technical Meeting and Exhibition Swaziland, 16 - 18 September 2009, pages 490 - 499 Revealing the Beattie Magnetic Anomaly and the anatomy of the crust of southernmost Africa: Geophysics and deep sub- surface geology where the Cape Fold Belt and Karroo Basin meet A. S. Lindeque1,2,3, M.J. de Wit4 1. Now at Alfred Wegener Institute for Polar and Marine Research, Geophysics, Building D3280, Am Alten Hafen 26, 27568 Bremerhaven, Germany, [email protected] 2. Council for Geoscience, Western Cape, P.O. Box 572, Bellville 7535, Cape Town, South Africa 3. GeoForschungsZentrum Potsdam, Section 2.2, Telegrafenberg, 14473 Potsdam, Germany 4. AEON - Africa Earth Observatory Network and Department of Geological Sciences, University of Cape Town, Rondebosch 7701, South Africa, [email protected] ABSTRACT The deep crust of the southernmost margin of Africa contains unresolved tectonic features such as the Paleozoic Cape Fold Belt (CFB), the Paleozoic-Mesozoic Karroo Basin and the largest terrestrial magnetic anomaly, the Beattie Magnetic Anomaly (BMA). Without resolving these structures, our understanding of the evolution of the southern margin will be incomplete and limited. Under the auspices of the Inkaba yeAfrica framework, several geophysical datasets were acquired from 2004 to 2007, along two transects across the margin and its unique tectonic features. This research presents a tectonic model and crustal geometry, at the centre 100 km of the western transect. The model is derived from the joint interpretation of: surface geology, aeromagnetic data, nearby deep boreholes, teleseismic receiver functions, impedance spectroscopy measurements on borehole samples, near vertical reflection seismic data (NVR), shallow P- and S-wave velocity data, wide angle refraction data and magnetotelluric data. -
Ecca Group) of South Africa: a Preliminary Review of Palaeoniscoid Fishes and Taphonomy
Records of the Western Australian Museum Supplement No. 57: 175-181 (1999). The Permian Whitehill Formation (Ecca Group) of South Africa: a preliminary review of palaeoniscoid fishes and taphonomy Fiona J. Evans 1 and Patrick A. Bender2 I Department of Zoology, University of Stellenbosch, Private Bag Xl, Matieland, 7602, South Africa; email: [email protected] 2 Museum of the Council for Geoscience, Private Bag Xl12, Pretoria, 0001, South Africa Abstract - The Permian (Artinskian) Whitehill Formation (Ecca Group) in South Africa and southern Namibia was deposited as part of a large stratified inland sea which extended from the southern margins of South Africa, and southern Namibia, northern Namibia (Aba-Huab Formation, Huab Basin) to the Iratl Formation of the Parana Basin in Brazil and parts of Uruguay. A common biota exists between these two continents, namely mesosaurid reptiles, pygocephalomorph crustacea, wood, palaeoniscoid fish and insects. The Whitehill Formation also contains plant stem fragments, palynomorphs, coprolites, a cephalochordate, rare sponge spicules and traces of arthropods and fish. The good preservation, particularly of the palaeoniscoid material, from the Whitehill Formation contrasts strongly with the disarticulated scales and spines from northern Namibia and Brazil. Recent collections in the Whitehill Formation near Calvinia and Louriesfontein (Northern Cape Province) of South Africa have demonstrated the necessity for a review of the palaeoniscoid taxa present in these units. Possible new species have also been collected, including a deep-bodied form. INTRODUCTION The extensive stratified inland sea in which the Whitehill Formation (Ecca Group, Karoo Supergroup; - - - - - Waterford Fm Figure 1) was deposited had limited or no access to ------------ the ocean according to reconstructions by Oelofsen Fort Brown Fm and Araujo (1987) and Pickford (1995). -
Proposed Limestone Quarry on Portion 1Of East of Gous Kraal No. 257
PALAEONTOLOGICAL IMPACT ASSESSMENT: DESKTOP STUDY Proposed limestone quarry on Portion 1 of East of Gous Kraal No. 257, Cacadu District, Eastern Cape John E. Almond PhD (Cantab.) Natura Viva cc, PO Box 12410 Mill Street, Cape Town 8010, RSA natu [email protected] April 2009 1. SUMMARY The proposed new limestone quarry north of Mount Stuart (Steytlerville area, Eastern Cape) will entail shallow excavations into potentially fossil-bearing mudrocks of the Early Permian (278 Ma) Whitehill Formation. The most important fossils likely to be found here include aquatic mesosaurid reptiles, primitive bony fishes and crustaceans. However, the overall impact of the development on palaeontological resources is likely to be minor since unweathered bedrock is unlikely to be exploited and the planned quarrying activities are both small-scale and short-term. Further specialist palaeontological mitigation is therefore not recommended. Should fossil remains be encountered during excavation, however, the material should be safeguarded and SAHRA or a local museum be contacted for advice by the responsible ECO. 2. INTRODUCTION & BRIEF SA Lime (Eastern Cape) (Pty) Ltd are proposing to quarry limestone for agricultural lime on Portion 1 of the farm East of Gous Kraal No. 257, situated c. 25km northwest of Steyllerville in the Eastern Cape (Ikwezi Magesterial Area, Cacadu District). The new quarry will be located on the west side of the R338 and some 3 km north of the hamlet of Mount Stuart (Fig. 1). It will be in operation for about five months and will only involve an area of 150m X 100m. An existing quarry that has been operated by PPC since 1965 is situated on the opposite side of the R338 road. -
South African Journal of Science Volume 113 | Number 3/4 1 March/April 2017 Invited Commentary Mathematics in Mathematics Education Page 1 of 3
Synergies in the mathematical SOUTH AFRICAN sciences Journal of Science Alternative age for Little Foot Characterisation of traditional cosmetic clays Determination of ancient arrow poisons ISSN: 1996-7489 e MARCH/APRIL 2017 volume 113 number 3/4 MARCH/APRIL eISSN: 1996-7489 EDITOR-IN-CHIEF John Butler-Adam Office of the Vice Principal: Research and Graduate Education, University of Pretoria SOUTH AFRICAN MANAGING EDITOR Linda Fick Academy of Science of South Africa Journal of Science ONLINE PUBLISHING ADMINISTRATOR volume 113 Nadine Wubbeling Academy of Science of South Africa number 3/4 ASSOCIATE EDITORS Sally Archibald School of Animal, Plant & Environmental Sciences, University of the Witwatersrand Leader Nicolaas Beukes Mathematics and… Department of Geology, University of Johannesburg John Butler-Adam .................................................................................................................... 1 Tania Douglas Invited Commentary Division of Biomedical Engineering, University of Cape Town Mathematics in mathematics education Jill Adler .................................................................................................................................. 2 Menán du Plessis Department of General Linguistics, Finding synergies between the mathematical and physical sciences Stellenbosch University Daya Reddy ............................................................................................................................. 5 Kavilan Moodley Mathematics and biology School of Mathematics, Statistics