SOME MAIN CONCLUSIONS DRAWN FROM A BASINAL ANALYSIS OF THE DWYKA SERIES IN THE KARROO BASIN
| dc.contributor.author | Stratten, T. | |
| dc.date.accessioned | 2014-09-22T11:25:31Z | |
| dc.date.available | 2014-09-22T11:25:31Z | |
| dc.date.issued | 1968 | |
| dc.description.abstract | The 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. | en_ZA |
| dc.description.sponsorship | Union Corporation, Limited | en_ZA |
| dc.identifier.issn | 0078-8554 | |
| dc.identifier.uri | http://hdl.handle.net/10539/15584 | |
| dc.language.iso | en | en_ZA |
| dc.publisher | BERNARD PRICE INSTITUTE FOR PALAEONTOLOGICAL RESEARCH | en_ZA |
| dc.title | SOME MAIN CONCLUSIONS DRAWN FROM A BASINAL ANALYSIS OF THE DWYKA SERIES IN THE KARROO BASIN | en_ZA |
| dc.type | Article | en_ZA |
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