Zobrazeno 1 - 10
of 37
pro vyhledávání: '"J.W. Bristow"'
Autor:
F.J. Venter, J.W. Bristow
Publikováno v:
Koedoe: African Protected Area Conservation and Science, Vol 29, Iss 1, Pp 117-124 (1986)
An outline is presented of the geomorphic history as well as the present terrain morphology and drainage of the Kruger National Park which forms part of the eastern Transvaal Lowveld. The Lowveld represents the footslope of the Drakensberg, the escar
Externí odkaz:
https://doaj.org/article/58bed72082e8489fa4618e3cfe3c5960
Autor:
J.W. Bristow
Publikováno v:
Koedoe: African Protected Area Conservation and Science, Vol 29, Iss 1, Pp 59-67 (1986)
Volcanic and sedimentary rocks occupy a faulted graben within the previously uplifted and eroded high-grade gneiss terrain of the Limpopo Mobile Belt. The rocks comprise the Soutpansberg Group and represent an important sequence of Proterozoic rocks.
Externí odkaz:
https://doaj.org/article/a7259bf29fec4cc1a55d53d02234b01e
Publikováno v:
Koedoe: African Protected Area Conservation and Science, Vol 29, Iss 1, Pp 39-44 (1986)
Precambrian granitoid rocks underlie approximately 60 percent of the Kruger National Park. They occur primarily in the western portion of the park and comprise a wide variety of rock including granites, granodiorites, tonalites, trondhjemites and sye
Externí odkaz:
https://doaj.org/article/ce7f683c9f3b4369ac20ca73f21f82d1
Publikováno v:
Koedoe: African Protected Area Conservation and Science, Vol 29, Iss 1, Pp 183-202 (1986)
The Kruger National Park (KNP) contains a considerable variety of rock types, ranging from Archaean granitoids to Recent sedimentary deposits. Some 3 500 million years of geological history is represented in an approximately 85 km east-west section a
Externí odkaz:
https://doaj.org/article/63ab0de1646d46638deaffbdd8936aad
Autor:
J.W. Bristow, F.J. Venter
Publikováno v:
Koedoe: African Protected Area Conservation and Science, Vol 29, Iss 1, Pp 85-104 (1986)
Permian to Recent rocks form narrow, roughly north- south and east-south-east trending belts in the north-eastern Transvaal. The rocks consist of a thin succession of Karoo sediments, a thick overlying succession of mafic and felsic volcanics referre
Externí odkaz:
https://doaj.org/article/ef1c4fb9914c433e9a1ddbb5cb6bdbcc
Publikováno v:
South African Journal of Geology. 125:225-243
The Bumbeni Complex represents an Early Cretaceous volcanic complex that developed at the southern termination of the Lebombo mountain range in northern KwaZulu-Natal, South Africa. The volcano-sedimentary complex intrudes and disconformably overlies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e4907d472ff452e32f35dd877e32848
https://doi.org/10.25131/sajg.125.0012
https://doi.org/10.25131/sajg.125.0012
Akademický článek
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Akademický článek
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K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
F.J. Venter, J.W. Bristow
Publikováno v:
Koedoe: African Protected Area Conservation and Science, Vol 29, Iss 1, Pp 85-104 (1986)
Permian to Recent rocks form narrow, roughly north- south and east-south-east trending belts in the north-eastern Transvaal. The rocks consist of a thin succession of Karoo sediments, a thick overlying succession of mafic and felsic volcanics referre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10272a4d4b2872c560407e94d8d380e5
https://koedoe.co.za/index.php/koedoe/article/view/522
https://koedoe.co.za/index.php/koedoe/article/view/522
Publikováno v:
Koedoe: African Protected Area Conservation and Science, Vol 29, Iss 1, Pp 183-202 (1986)
The Kruger National Park (KNP) contains a considerable variety of rock types, ranging from Archaean granitoids to Recent sedimentary deposits. Some 3 500 million years of geological history is represented in an approximately 85 km east-west section a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::302e04671fee3879a00f4d66657b14f7
https://koedoe.co.za/index.php/koedoe/article/view/530
https://koedoe.co.za/index.php/koedoe/article/view/530