Geochemistry of Karoo basalts and dolerites in the northeastern Orange Free State: Recognition and origin of the new Karoo basalt magma types.
- Authors: Marsh, J S
- Date: 1984
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/71283 , vital:29829
- Description: One of the most significant results emerging from the Karoo Volcanics Project of the NGP ls the recognition of a number of geochemically distinct basalt magma types occurring within the lower part of the Karoo volcanic pile in the Northeastern Cape and Southern Lesotho.
- Full Text: false
- Date Issued: 1984
- Authors: Marsh, J S
- Date: 1984
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/71283 , vital:29829
- Description: One of the most significant results emerging from the Karoo Volcanics Project of the NGP ls the recognition of a number of geochemically distinct basalt magma types occurring within the lower part of the Karoo volcanic pile in the Northeastern Cape and Southern Lesotho.
- Full Text: false
- Date Issued: 1984
Geochemistry of Karoo basalts and dolerites in the northeastern Orange Free State: Recognition and origin of the new Karoo basalt magma types.
- Authors: Marsh, J S
- Date: 1984
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/71288 , vital:29830
- Description: One of the most significant results emerging from the Karoo Volcanics Project of the NGP ls the recognition of a number of geochemically distinct basalt magma types occurring within the lower part of the Karoo volcanic pile in the Northeastern Cape and Southern Lesotho.
- Full Text:
- Date Issued: 1984
- Authors: Marsh, J S
- Date: 1984
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/71288 , vital:29830
- Description: One of the most significant results emerging from the Karoo Volcanics Project of the NGP ls the recognition of a number of geochemically distinct basalt magma types occurring within the lower part of the Karoo volcanic pile in the Northeastern Cape and Southern Lesotho.
- Full Text:
- Date Issued: 1984
Petrogenesis of Karoo magmas from Namibia and the nature of their source areas
- Authors: Marsh, J S , Miller, R
- Date: 1982
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/71299 , vital:29831
- Full Text:
- Date Issued: 1982
- Authors: Marsh, J S , Miller, R
- Date: 1982
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/71299 , vital:29831
- Full Text:
- Date Issued: 1982
The geochemistry of basic volcanics of the Dordabis Formation northeast of Dordabis and their significance for correlations within, and evolution of, the Rehoboth Magmatic Arc
- Marsh, J S, Williams-Jones, I E
- Authors: Marsh, J S , Williams-Jones, I E
- Date: 1985
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/69763 , vital:29577 , http://www.mme.gov.na/files/publications/95f_Williams-Jones and Marsh_Dordabis Fm.pdf
- Description: Gevers (1934) named the succession of quartzites, feld-spathic sandstones, massive conglomeratic arkoses and sedimentary breccias around Dordabis, the Dordabis Series. He considered this series to be of Nama age and the basic volcanics in the series to be post Nama, pre-Karoo eruptive diabase. Schalk (pers. comm.) has found the succession to be pre-Damara in age and possibly equivalent to the Sinclair Sequence. These ‘Dordabis Series’ rocks have since been incorrectly included into the Marienhof Formation of the Rehoboth Sequence on the 1980 1:1 000 000 Geological Map of SWA/Namibia. In this report, it is suggested that this succession be called the Dordabis Formation.
- Full Text:
- Date Issued: 1985
- Authors: Marsh, J S , Williams-Jones, I E
- Date: 1985
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/69763 , vital:29577 , http://www.mme.gov.na/files/publications/95f_Williams-Jones and Marsh_Dordabis Fm.pdf
- Description: Gevers (1934) named the succession of quartzites, feld-spathic sandstones, massive conglomeratic arkoses and sedimentary breccias around Dordabis, the Dordabis Series. He considered this series to be of Nama age and the basic volcanics in the series to be post Nama, pre-Karoo eruptive diabase. Schalk (pers. comm.) has found the succession to be pre-Damara in age and possibly equivalent to the Sinclair Sequence. These ‘Dordabis Series’ rocks have since been incorrectly included into the Marienhof Formation of the Rehoboth Sequence on the 1980 1:1 000 000 Geological Map of SWA/Namibia. In this report, it is suggested that this succession be called the Dordabis Formation.
- Full Text:
- Date Issued: 1985
The Klinghardt phonolites, South West Africa: Tertiary volcanism in western southern Africa
- Authors: Marsh, J S , Lock, B E
- Date: 1975
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/70164 , vital:29627
- Description: Over 1OO phonolite bodies of mid-Tertiary age occur in the Klinghardt Mountains, 1OO km SE of Luderitz in Southern South West Africa the only published account of these rocks is that of Kaiser (1926) who gives a generalized map and describes briefly the mode of occurrence and petrography of the phonolites. The phonolite bodies are concentrated in an area roughly 8OO km2 and constitute an excellent example of an areal volcanic field (Rittmann, 1962), i.e. the activity occurred at a number of vents spread over a wide area and in most cases only a single eruptive episode took place at each vent.
- Full Text:
- Date Issued: 1975
- Authors: Marsh, J S , Lock, B E
- Date: 1975
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/70164 , vital:29627
- Description: Over 1OO phonolite bodies of mid-Tertiary age occur in the Klinghardt Mountains, 1OO km SE of Luderitz in Southern South West Africa the only published account of these rocks is that of Kaiser (1926) who gives a generalized map and describes briefly the mode of occurrence and petrography of the phonolites. The phonolite bodies are concentrated in an area roughly 8OO km2 and constitute an excellent example of an areal volcanic field (Rittmann, 1962), i.e. the activity occurred at a number of vents spread over a wide area and in most cases only a single eruptive episode took place at each vent.
- Full Text:
- Date Issued: 1975
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