ARE DIAMICTITES IMPACT EJECTA - NO SUPPORTING EVIDENCE FROM SOUTH-AFRICAN DWYKA GROUP DIAMICTITE

Citation
Wu. Reimold et al., ARE DIAMICTITES IMPACT EJECTA - NO SUPPORTING EVIDENCE FROM SOUTH-AFRICAN DWYKA GROUP DIAMICTITE, The Journal of geology, 105(5), 1997, pp. 517-530
Citations number
66
Categorie Soggetti
Geology
Journal title
ISSN journal
00221376
Volume
105
Issue
5
Year of publication
1997
Pages
517 - 530
Database
ISI
SICI code
0022-1376(1997)105:5<517:ADIE-N>2.0.ZU;2-Y
Abstract
Diamictites, especially those deposited before the break-up of Gondwan a in the Late Carboniferous and Permian, have recently been suggested to represent ejecta deposits from large comet or meteorite impact even ts. This is in contrast to the commonly held interpretation that these rocks represent glaciomarine sedimentary deposits. To test this contr oversial hypothesis, we carried out a detailed petrographical study of over 75,000 mineral and rock clasts from a large number of Dwyka Grou p diamictite samples from localities covering an extensive part of the Karoo basin in southern Africa. No definitive evidence of impact-diag nostic shock metamorphic deformation in mineral or Lithic clasts from any of these samples was detected. We conclude, therefore, that to dat e no unequivocal evidence for an impact origin of these diamictites in the South African stratigraphic record has been documented. What is m ore, the general hypothesis that some diamictites in the stratigraphic record could represent impact ejecta is not supported by first-order observations of bona fide shock (impact) related phenomena in such roc ks.