Evidence from Dwyka tillite cobbles of Archaean basement beneath the Kalahari sands of southern Africa
(2011) In Lithos 125(1-2). p.482-502- Abstract
- We have found a new source of information about what lies beneath the Kalahari sands. The Kheis and Rehoboth Provinces of southern Africa were thought to be underlain by either an similar to 1800 Ma orogenic belt, or a northern branch of the similar to 1200 Ma Namaqua-Natal Province. Glacial diamictites of the Permocarboniferous Dwyka Group exposed at Rietfontein west of the Kalahari sands carry cobbles plucked from the bedrock by the ice sheet which covered the Gondwana supercontinent about 300 Ma ago. Despite altered mineralogy, the cobbles are not severely altered geochemically. Their normative mineral compositions give classifications as trondhjemites and granites, supported by rare earth element diagrams. Microbeam U-Pb zircon dating... (More)
- We have found a new source of information about what lies beneath the Kalahari sands. The Kheis and Rehoboth Provinces of southern Africa were thought to be underlain by either an similar to 1800 Ma orogenic belt, or a northern branch of the similar to 1200 Ma Namaqua-Natal Province. Glacial diamictites of the Permocarboniferous Dwyka Group exposed at Rietfontein west of the Kalahari sands carry cobbles plucked from the bedrock by the ice sheet which covered the Gondwana supercontinent about 300 Ma ago. Despite altered mineralogy, the cobbles are not severely altered geochemically. Their normative mineral compositions give classifications as trondhjemites and granites, supported by rare earth element diagrams. Microbeam U-Pb zircon dating of the granitic cobbles shows that they contain no evidence of crustal growth or orogeny at either 1800 or 1200 Ma. Rather they testify to the presence of 2500 to 2900 Ma Archaean trondhjemitic and granitic crust beneath the Kalahari, with a lesser similar to 2050 Ma granite component. The pebble assemblages from the diamictites we sampled lack the diagnostic banded iron formation (BIF), stromatolitic limestone and other supracrustal pebbles which characterise diamictites derived from the Kaapvaal Craton, thus we envisage shorter transport distances and derivation from the region now beneath the Kalahari sands. Three of the Archaean granite cobbles have unusual less-than-mantle zircon oxygen isotope values around +3 (delta(18)O VSMOW), which may reflect interaction of their source with high-temperature, originally meteoric water before melting to produce the granites. The mafic cobbles described in a companion paper are much younger and are related to intrusions of the 1.1 Ga Umkondo Large Igneous Province, probably located on the Kalahari Line or Rehoboth Province. Five trondhjemitic granites from the westernmost outcrops of the Kaapvaal Craton were dated, the oldest being 3061 +/- 9 Ma and four others between 2882 +/- 7 Ma and 2854 +/- 7 Ma, reflecting the cratonisation of the Kimberley Terrane. Four of the Archaean Dwyka cobbles we dated are younger than the 2.7 Ga Kaapvaal cover sequence and are thus too young to be derived from the craton. All the Dwyka cobbles described here are most likely derived from either the Rehoboth Province or the Kalahari Line with origins from the Kheis Province, Kaapvaal Craton, or further afield considered unlikely. We envisage the Rehoboth Province to consist of an Archaean core supplemented by Palaeoproterozoic granitoids, which was joined to the Kaapvaal Craton at an early stage of crustal development and played an important role during later tectonic events. This has important implications not only for the tectonic framework and assembly of Southern Africa, but also for exploration for diamonds and other ore deposits. (C) 2011 Elsevier B.V. All rights reserved. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/5051061
- author
- Cornell, David H. ; van Schijndel, Valby ; Ingolfsson, Olafur ; Scherstén, Anders LU ; Karlsson, Linn ; Wojtyla, Joanna and Karlsson, Kristin
- publishing date
- 2011
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- Kalahari, Dwyka Formation, Rehoboth Province, Kaapvaal Craton, Ion probe, zircon dating, Zircon oxygen isotope
- in
- Lithos
- volume
- 125
- issue
- 1-2
- pages
- 482 - 502
- publisher
- Elsevier
- external identifiers
-
- wos:000292663600031
- scopus:79958780849
- ISSN
- 0024-4937
- DOI
- 10.1016/j.lithos.2011.03.006
- language
- English
- LU publication?
- no
- id
- c8195761-fa4c-44f2-a873-ad369b3307dc (old id 5051061)
- date added to LUP
- 2016-04-01 10:43:28
- date last changed
- 2022-04-04 20:44:34
@article{c8195761-fa4c-44f2-a873-ad369b3307dc,
abstract = {{We have found a new source of information about what lies beneath the Kalahari sands. The Kheis and Rehoboth Provinces of southern Africa were thought to be underlain by either an similar to 1800 Ma orogenic belt, or a northern branch of the similar to 1200 Ma Namaqua-Natal Province. Glacial diamictites of the Permocarboniferous Dwyka Group exposed at Rietfontein west of the Kalahari sands carry cobbles plucked from the bedrock by the ice sheet which covered the Gondwana supercontinent about 300 Ma ago. Despite altered mineralogy, the cobbles are not severely altered geochemically. Their normative mineral compositions give classifications as trondhjemites and granites, supported by rare earth element diagrams. Microbeam U-Pb zircon dating of the granitic cobbles shows that they contain no evidence of crustal growth or orogeny at either 1800 or 1200 Ma. Rather they testify to the presence of 2500 to 2900 Ma Archaean trondhjemitic and granitic crust beneath the Kalahari, with a lesser similar to 2050 Ma granite component. The pebble assemblages from the diamictites we sampled lack the diagnostic banded iron formation (BIF), stromatolitic limestone and other supracrustal pebbles which characterise diamictites derived from the Kaapvaal Craton, thus we envisage shorter transport distances and derivation from the region now beneath the Kalahari sands. Three of the Archaean granite cobbles have unusual less-than-mantle zircon oxygen isotope values around +3 (delta(18)O VSMOW), which may reflect interaction of their source with high-temperature, originally meteoric water before melting to produce the granites. The mafic cobbles described in a companion paper are much younger and are related to intrusions of the 1.1 Ga Umkondo Large Igneous Province, probably located on the Kalahari Line or Rehoboth Province. Five trondhjemitic granites from the westernmost outcrops of the Kaapvaal Craton were dated, the oldest being 3061 +/- 9 Ma and four others between 2882 +/- 7 Ma and 2854 +/- 7 Ma, reflecting the cratonisation of the Kimberley Terrane. Four of the Archaean Dwyka cobbles we dated are younger than the 2.7 Ga Kaapvaal cover sequence and are thus too young to be derived from the craton. All the Dwyka cobbles described here are most likely derived from either the Rehoboth Province or the Kalahari Line with origins from the Kheis Province, Kaapvaal Craton, or further afield considered unlikely. We envisage the Rehoboth Province to consist of an Archaean core supplemented by Palaeoproterozoic granitoids, which was joined to the Kaapvaal Craton at an early stage of crustal development and played an important role during later tectonic events. This has important implications not only for the tectonic framework and assembly of Southern Africa, but also for exploration for diamonds and other ore deposits. (C) 2011 Elsevier B.V. All rights reserved.}},
author = {{Cornell, David H. and van Schijndel, Valby and Ingolfsson, Olafur and Scherstén, Anders and Karlsson, Linn and Wojtyla, Joanna and Karlsson, Kristin}},
issn = {{0024-4937}},
keywords = {{Kalahari; Dwyka Formation; Rehoboth Province; Kaapvaal Craton; Ion probe; zircon dating; Zircon oxygen isotope}},
language = {{eng}},
number = {{1-2}},
pages = {{482--502}},
publisher = {{Elsevier}},
series = {{Lithos}},
title = {{Evidence from Dwyka tillite cobbles of Archaean basement beneath the Kalahari sands of southern Africa}},
url = {{http://dx.doi.org/10.1016/j.lithos.2011.03.006}},
doi = {{10.1016/j.lithos.2011.03.006}},
volume = {{125}},
year = {{2011}},
}