Rhodes University Graduation Ceremony 1986
- Authors: Rhodes University
- Date: 1986
- Language: English
- Type: text
- Identifier: vital:8120 , http://hdl.handle.net/10962/d1005703
- Description: Rhodes University Graduation Ceremonies on Friday, 11 April 1986 at 8 p.m. [and] on Saturday, 12 April 1986 at 10 a.m. in the 1820 Settlers National Monument.
- Full Text:
- Date Issued: 1986
- Authors: Rhodes University
- Date: 1986
- Language: English
- Type: text
- Identifier: vital:8120 , http://hdl.handle.net/10962/d1005703
- Description: Rhodes University Graduation Ceremonies on Friday, 11 April 1986 at 8 p.m. [and] on Saturday, 12 April 1986 at 10 a.m. in the 1820 Settlers National Monument.
- Full Text:
- Date Issued: 1986
Volcanic rocks of the Witwatersrand triad, South Africa I: description, classification and geochemical stratigraphy
- Bowen, Teral B, Marsh, Julian S, Bowen, Michael P, Eales, Hugh V
- Authors: Bowen, Teral B , Marsh, Julian S , Bowen, Michael P , Eales, Hugh V
- Date: 2003
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/138682 , vital:37663 , https://doi.org/10.1016/0301-9268(86)90038-0
- Description: The Witwatersrand triad contains thick volcanic sequences confined largely to the Dominion Group at the base and the Ventersdorp Supergroup at the top. These volcanic sequences are of late-Archaean to early-Proterozoic age and are amongst the oldest supracrustal volcanic sequences erupted onto the Archaean Kaapvaal craton. The volcanic rocks have suffered low-grade greenschist facies metamorphism but primary textures and, in some samples, primary mineralogies are well preserved.
- Full Text: false
- Date Issued: 2003
- Authors: Bowen, Teral B , Marsh, Julian S , Bowen, Michael P , Eales, Hugh V
- Date: 2003
- Language: English
- Type: text , article
- Identifier: http://hdl.handle.net/10962/138682 , vital:37663 , https://doi.org/10.1016/0301-9268(86)90038-0
- Description: The Witwatersrand triad contains thick volcanic sequences confined largely to the Dominion Group at the base and the Ventersdorp Supergroup at the top. These volcanic sequences are of late-Archaean to early-Proterozoic age and are amongst the oldest supracrustal volcanic sequences erupted onto the Archaean Kaapvaal craton. The volcanic rocks have suffered low-grade greenschist facies metamorphism but primary textures and, in some samples, primary mineralogies are well preserved.
- Full Text: false
- Date Issued: 2003
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