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REPUBLIC OF SOUTH AFRICA DEPARTMENT OF MINES GEOLOGICAL SURVEY THE GEOLOGY OF THE COUNTRY AROUND PRETORIA AN .EXPLANATION OF SHEETS 2527DA, DB, DC, DD AND 2528CA, CB, CC, CD compiled by H. JANSEN, D.Sc. COPYRIGHT RESERVED 1977 Printed by and obtainable (rom The Government Printer, Bosman Street, …
A set of ten en echelon felsite sills is exposed in the East Rand Proprietary Mines, Boksburg. These sills are part of a larger occurrence of felsite sills which occur in the Witwatersrand, and …
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ABSTRACT The 2150 Ma Rooiberg Felsite Group, Transvaal Sequence, contains thin sandstone interbeds within its 3500-5000 m thick volcanic succession. Whereas uppermost feldspathic arenites and wackes are thought to represent reworked felsitic material, quartz arenites and subordinate lithic sandstones, present throughout most of the Rooiberg sequence, …
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The BC consists of the basal Rooiberg felsite, the ultramafic to mafic suite, which is ... The inset map shows the location of the Bushveld Complex in South Africa. The TML stands for Thabazimbi–Murchison–Lineament, while EL, WL, NL, FWL, VLN and BL are eastern and western limbs, northern lobe, far-western limb, Villa Nora and Bethal limb ...
Abstract.The volcanic Rooiberg Group represents the earliest phase of Bushveld-related magmatism and comprises, in some areas, the floor and roof rocks of the mafic–ultramafic intrusive units of the Bushveld Complex. The lower to middle Dullstroom Formation is composed of two interbedded series of low Ti and high Ti volcanic strata, which are predominantly …
Quaternary international, 2005. South of the modern Limpopo River near its confluence with the Shashe, gravels associated with an ancient aggrading terrace of the river attracted Earlier Stone Age (ESA) occupations preserved in the Vhembe-Dongola National Park of South Africa.
Drill core from a fence of five boreholes located in the vicinity of Roossenekal, in the eastern limb of the Bushveld Complex, South Africa, provides complete coverage of what is probably one of the thickest and most well-developed sections of the Upper Zone.
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It has been suggested that the Bushveld Complex of South Africa could be the result of multiple large meteorite or comet impacts. According to this hypothesis, part of the …
in the north and by Rooiberg Felsite and sediments of the Waterberg Group in the south. According to interpreted gravity values on the flank of the Dennilton dome, rocks of the Transvaal Supergroup which outcrop on the south-eastern flank of the dome, have been intruded by mafic rocks of the Bushveld Complex.
The Bushveld Complex is situated in the central Transvaal, South Africa, and covers an area of 67,000 km 2 of which about one-third is concealed by younger formations ().It consists of a large variety of extrusive, intrusive, and metamorphic rocks, the basic stratified portion of which constitutes the largest layered intrusion of its kind in the world.
Wagner was born in South Africa and educated in Cape Town. Field mapping undertaken over 29 years enabled Hall to produce the only comprehensive field guide to the Eastern Limb (Hall 1932 ). Recent guidebooks with selected geosites include those by Sharpe ( 1986 ) and Scoon ( 2016 ).
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The mafic Bushveld Complex is divided into five limbs (far western, western, southern, eastern and northern). b Geological map of the eastern limb of the Bushveld Complex showing the …
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Introduction. The historic Waterberg platinum deposit – not related to the current 'Waterberg Project' exploration being carried out by Platinum Group Metals Ltd. in the far north of the northern limb of the Bushveld Complex – is located some 15 km WNW of Mookgophong (formerly Naboomspruit) in the Waterberg District, Limpopo Province, South Africa ().
Dolerite sills. Associated with the vast outpouring of lava there was a huge deep plumbing system of molten rock, called magma.Magmas originated by melting at depths of 100 km inside the Earth ...
One type, the so-called "Rooiberg granophyre", is found as large sheet-like bodies at the base of the Rooiberg felsite in the area investigated, and is considered to have originated by melting of …
Fluorine Fluorite mining deposit report for "Deposit #22793" (#22793) in Limpopo, South Africa.
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The Nebo granite (Bushveld granite) occupies extensive areas in the central portion of the Complex, where it is intrusive into felsite, granophyre, and leptite. The latter two usually …
A wide variety of silicic rocks are found in continental LIPs that include (dominantly) rhyolite, dacite, felsite, trachyte, trachydacite, rhyodacite, silicic ignimbrite, quartz latite, comendite, pantellerites, granophyre, pitchstone, obsidian, and silicic porphyry (Supplementary Table 1).Many of these rock types, as described in the literature, are lithological (e.g., …
Paardekop consist of highly metamorphosed felsite, generally referred to as leptite, relatively unaltered felsite and granophyre which occurs as a thick sill between the leptite and the felsite. …
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The geological succession of an area in the southeastern Bushveld Complex, South Africa is described here, in which up to 700 m of monzonitic rocks, more evolved than in …
The ∼2.06 Ga Rooiberg Group of South Africa, related to the greater Bushveld Complex-forming event (Bushveld Large Igneous Province) appears to have been associated with some of the largest eruptions of silicic rocks in the Precambrian rock record.Despite extensive geochemical work that has been carried out on the voluminous silicic volcanic and intercalated …
The Bushveld Complex of South Africa consists of three suites of igneous rocks: the layered mafic and ultramafic rocks of the Rustenburg Layered Suite (RLS), granites of the …
Other articles where Bushveld Complex is discussed: Africa: The Precambrian: …2 billion years ago the Bushveld Complex—which is one of the largest differentiated igneous bodies on Earth, containing major deposits of platinum, chromium, and vanadium—was emplaced in the northern Kaapvaal craton. The middle part of the early Proterozoic was dominated by powerful orogenic …
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