Conveners
Minerals: Session Chair: Dr. Marco Andreoli
- Marco Andreoli (Necsa; University of hte Witwatersrand)
Minerals
- Marco Andreoli (Necsa; University of hte Witwatersrand)
Mr
Tshipeng Mwenze
(University of the Western Cape)
02/10/2014, 09:45
Oral and Poster Presentation
The paucity of geochemical criteria for stratigraphic correlations and defining the styles of mineralisation pose serious problems in locating PGE-rich zones in the Platreef. This study is therefore aimed at identifying and appraising process-based mineralogical/ geochemical criteria which may be useful in stratigraphic correlations and characterizing the nature and styles of PGE...
Mr
Hakundwi Mandende
(University of the Western Cape)
02/10/2014, 10:00
Oral and Poster Presentation
The Platreef is located in the northern limb of the Bushveld Igneous Complex (BIC) and is comprised of a 10- to 400-m thick package of pyroxenitic lithologies, which host platinum-group element (PGE) and base metal sulphide (BMS) mineralization at various heights above the floor rocks. The pyroxenites are overlain by norites and gabbronorites, generally assigned to the Main Zone of the BIC....
Ms
Jarlen Beukes
(University of the Free State)
02/10/2014, 10:15
Oral and Poster Presentation
This research study focuses on the enigmatic occurrence of noritic lenses (termed “brown sugar norite” by mine geologists, here after referred to as BSN), within the feldspathic pyroxenite of the Merensky Reef (MR) at Two Rivers Platinum Mine which is situated on the southern sector of the eastern limb of the Bushveld Complex. The cumulate rocks associated with the MR unit are characterised by...
Mr
Reddy Bokana
(University of the Western Cape (Applied Geology))
02/10/2014, 11:00
Oral and Poster Presentation
The Hondekloof deposit represents a family of small, orthomagmatic massive sulphide Ni-Cu-(Co-Zn) deposits occurring in the central part of the Garies terrane, Bushmanland, Namaqualand, South Africa. The study area is located in the Westcoast region of South Africa, in the settlement called Kliprand where various granulite facies rocks of the Namaqua-Natal Metamorphic province ranging from...
Mr
Roberto Almanza
(Nelson Mandela Metropolitan Univeristy)
02/10/2014, 11:15
Oral and Poster Presentation
The Steyterville-Jansenville gypsum field is one of South Africa’s smaller deposits. It is covered by an average of 500mm of soil and has fine powdery gypsum bodies which are, on average, 37cm thick and contain an average of 65% gypsum – medium grade. The calcium and sulphate ions required to form the gypsum mineral (CaSO4•2H2O) are supplied by the Whitehill Formation shale which is carbonate...
Mr
Pule Petrus Molokoane
(University of the Free State)
02/10/2014, 11:30
Oral and Poster Presentation
Pseudo first order oxidation of 3,5-di-tert-butylcatechol under aerobic conditions to 3,5-di-tert-butylquinone. The process was catalyzed by square planar Cu(II)(naltol)2 complexes. The aim of this study was to imitate the activity and behaviour of the enzyme catechol oxidase by employing copper nano molecular materials, and to investigate electronic and steric effects on this catalytic...
Mr
Adrian Adams
(University of Stellenbosch)
02/10/2014, 11:45
Oral and Poster Presentation
Atrazine, a popular herbicide, endocrine disruptor and possible carcinogen, is frequently detected in water systems. Its biodegradation in soils is well documented, but its degradation on soil mineral surfaces is only partially understood. Furthermore, changing global climate and increased temperatures could possibly increase occurrences of extreme drying (evaporation) in soils, a process...
Mr
Oluseyi Abegunde
(University of the Western Cape)
02/10/2014, 12:00
Oral and Poster Presentation
This study evaluated the magnitude of possibly leachable metals and predicted the AMD discharge over time, from Mogale tailings dam into the environs in Randfontein area, Witwatersrand Basin, South Africa. Drill core samples were analysed for multi-elements and evaluated using multivariate statistical and geochemical mass balance techniques.
The tailings dam lithology was grouped into four...