Here is a prograding deep-water basin floor fans succession from the Laingsburg depocentre and lovely diamictites from the underlying glacial Carboniferous Dwyka Group pic.twitter.com/OU5MFdLaVw
— Kévin Boulesteix (@muddy_turbidite) March 11, 2019
via Twitter https://twitter.com/muddy_turbidite
March 11, 2019 at 09:15PM
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