Add to ORKGThe research fell mainly into two separate but related fields of study. The first field was to investigate the pre-Karroo surface with special reference to the geology beneath the Karroo System. The second field was to investigate the paleo-ice flow directions of the Dwyka Tillite and relate this to the position and lithology of the source areas.Union Corporation, Limite
Abstract: The Witwatersrand basin i a large hinterland basin of Archaean age developed on already co...
Thesis (MSc)--Stellenbosch University, 2015.ENGLISH ABSTRACT: Diamictites are sedimentary deposits t...
The locality of Zwartbas is situated at the border of Namibia and South Africa about 15 km west of N...
The early efforts of Booth, Johnson, Rubidge, Catuneanu, de Wit, Chevallier, Stankiewicz, Weckmann a...
International audienceAlong the easternmost edge of the Karoo-Kalahari Basin (KKB) of Botswana, the ...
The area investigated is situated in the district of Rustenburg, about 55 miles due north of the tow...
Thesis (PhD)--Stellenbosch University, 2020.ENGLISH ABSTRACT: This dissertation is a compilation of ...
International audienceThe Late Paleozoic Ice Age (LPIA) is the longest-lived and most extreme glacia...
The Cape Supergroup (Sequence) comprises three groups, embracing a total of twenty-three formations,...
An area of 4 400 km² in the North-western Transvaal is compared to an area of 75 000 km² in the Nort...
The Tshipise Basin is considered to be a fault bounded remnant of a larger Karoo aged basin that wa...
Concentrating on the Katberg and Burgersdorp Formations, this research examined the sedimentary envi...
The sedimentary rocks of the Karoo Supergroup in the Tuli Basin (South Africa) consist of various te...
The nature of the geology beneath the Karoo Supergroup in South Africa has been of considerable inte...
Current correlations between the Pretoria and Postmasburg Groups of the Transvaal Supergroup are sho...
Abstract: The Witwatersrand basin i a large hinterland basin of Archaean age developed on already co...
Thesis (MSc)--Stellenbosch University, 2015.ENGLISH ABSTRACT: Diamictites are sedimentary deposits t...
The locality of Zwartbas is situated at the border of Namibia and South Africa about 15 km west of N...
The early efforts of Booth, Johnson, Rubidge, Catuneanu, de Wit, Chevallier, Stankiewicz, Weckmann a...
International audienceAlong the easternmost edge of the Karoo-Kalahari Basin (KKB) of Botswana, the ...
The area investigated is situated in the district of Rustenburg, about 55 miles due north of the tow...
Thesis (PhD)--Stellenbosch University, 2020.ENGLISH ABSTRACT: This dissertation is a compilation of ...
International audienceThe Late Paleozoic Ice Age (LPIA) is the longest-lived and most extreme glacia...
The Cape Supergroup (Sequence) comprises three groups, embracing a total of twenty-three formations,...
An area of 4 400 km² in the North-western Transvaal is compared to an area of 75 000 km² in the Nort...
The Tshipise Basin is considered to be a fault bounded remnant of a larger Karoo aged basin that wa...
Concentrating on the Katberg and Burgersdorp Formations, this research examined the sedimentary envi...
The sedimentary rocks of the Karoo Supergroup in the Tuli Basin (South Africa) consist of various te...
The nature of the geology beneath the Karoo Supergroup in South Africa has been of considerable inte...
Current correlations between the Pretoria and Postmasburg Groups of the Transvaal Supergroup are sho...
Abstract: The Witwatersrand basin i a large hinterland basin of Archaean age developed on already co...
Thesis (MSc)--Stellenbosch University, 2015.ENGLISH ABSTRACT: Diamictites are sedimentary deposits t...
The locality of Zwartbas is situated at the border of Namibia and South Africa about 15 km west of N...