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
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.