HG 186.9-187.0 D.E.


Autoria(s): Desconhecido
Data(s)

15/04/2015

15/04/2015

13/04/2015

Resumo

Coarse grained sediment with a few fine grained matrices. Brown sediment with small to medium sized clasts. Clasts range from sub-angular to sub-rounded. Organic material present. It contains rotation structures throughout as well as edge-to-edge grain crushing. Fine grained clay domains are present and lineations can also be seen. Minor amounts of grain stacking can also be seen.

Identificador

http://hdl.handle.net/10464/6259

Palavras-Chave #Rotation structures (without a central grain), edge-to-edge grain crushing
Tipo

Image