
Abstract
Lower Proterozoic stromatolites and associated clastic carbonate deposits of the Campbell Group, from the southern margin (Prieska area) of the Kaapvaal Craton, northern Cape Province, are described. Contrary to previous interpretations (Beukes, 1978; 1980a) shallow subtidal to supratidal facies are recognised and discussed in regional context. An alternative model for the facies development of the Campbell Group is proposed.
Item Type: | Journal article |
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Faculties: | Geosciences > Department of Earth and Environmental Sciences > Geology |
Subjects: | 500 Science > 550 Earth sciences and geology |
URN: | urn:nbn:de:bvb:19-epub-5456-8 |
Language: | English |
Item ID: | 5456 |
Date Deposited: | 06. Aug 2008, 16:08 |
Last Modified: | 04. Nov 2020, 12:48 |