Annals of the South African Museum: Annale Van Die Suid-Afrikaanse Museum |
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Page 218
Interpretation of this sequence is made difficult by the fact that it is abruptly truncated by a major erosion surface , but it is thought to be part of an inter - distributary bay fill ( Elliot 1974 ) . SEDIMENT .
Interpretation of this sequence is made difficult by the fact that it is abruptly truncated by a major erosion surface , but it is thought to be part of an inter - distributary bay fill ( Elliot 1974 ) . SEDIMENT .
Page 219
3. Stratigraphic log of about 100 m of strata in Howison's Poort , near Grahamstown . The major erosion surface marks the end of the constructional SEDIMENTARY FACIES IN THE LOWER WITTEBERG GROUP 219.
3. Stratigraphic log of about 100 m of strata in Howison's Poort , near Grahamstown . The major erosion surface marks the end of the constructional SEDIMENTARY FACIES IN THE LOWER WITTEBERG GROUP 219.
Page 220
The major erosion surface marks the end of the constructional phase of delta out - building and the remaining sediments of the Weltevrede Formation were deposited during a destructional phase . This involved transgressive marine ...
The major erosion surface marks the end of the constructional phase of delta out - building and the remaining sediments of the Weltevrede Formation were deposited during a destructional phase . This involved transgressive marine ...
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Common terms and phrases
abbreviated according articulate brachiopods association author's name authors Barwis bedding benthic assemblages bivalves Blinkberg Bokkeveld Group Boucot capital collected communities consists containing cycles delta deposited described Devonian Devonian rocks differences DISTRIBUTARY diversity dominated Eastern environment environmental fauna feeders figures gastropod given homalonotid Howison's Poort illustrations inarticulate indicate infaunal interpreted intertidal italics known letters Lingula localities lower major marine marine invertebrates mark Member Middle mould Museum Natural History nearshore Note occur original placed plant fossils Plectonotus possible punctuation quartz arenites range recorded references represent reworking salinity sandstones scientific sediment SEDIMENTARY FACIES separates sequence shales shallow siltstone similar Smith South African species specimens Stratigraphic subtidal suggest Tables Tankard thick thin Touws River trace fossils trilobite Tropidoleptus sp unit upper valve Wagen Drift Formation Weltevrede Formation Western Cape Witpoort Formation Witteberg Group yielded Zoophycos