907 resultados para stacking fault


Relevância:

10.00% 10.00%

Publicador:

Resumo:

Dark brown sediment with manly small sized clasts. Some medium and large clasts also present. Clasts range from sub-angular to sub-rounded. Lineations can be seen throughout the sample. Minor patches of clay/organic rich domains can also be seen as well as minor grain stacking.

Relevância:

10.00% 10.00%

Publicador:

Resumo:

Dark brown sediment with clasts ranging from small to medium in size and sub-angular to angular. Contains lineations and grain stacking throughout the sample. Rotation and comet structures can also be seen. Rotation structures can be seen around mainly the sub-angular clasts. Patches of clay can also be seen throughout the sample.

Relevância:

10.00% 10.00%

Publicador:

Resumo:

Dark brown sediment with sub-angular to sub-rounded clasts. Rotation structures and lineations are common. Clasts ranging from small to large in size. Many large grains are fractured. Minor amounts of grain stacking and crushing can be seen. A few clay and organic rich domains can be seen.

Relevância:

10.00% 10.00%

Publicador:

Resumo:

Coarse grained sample with clay stained domains. Grains range from small to medium in size and are sub-angular. Lineations, weathered grains, and minor grain stacking.

Relevância:

10.00% 10.00%

Publicador:

Resumo:

Coarse grained sediment with clasts ranging from small to medium in size. Clast shape range from sub-angular to sub-rounded. Lineations are present throughout the sample. Edge-to-edge grain crushing, grain stacking, and comet structures can also be seen. Some grains are crushed into one another. Areas of finer sediment can also be seen.

Relevância:

10.00% 10.00%

Publicador:

Resumo:

Coarse grained sample, with small clasts. Clasts range from sub-angular to sub-rounded in shape. Lineations are abundant throughout the sample. Grain stacking and crushing can also be seen in minor amounts.

Relevância:

10.00% 10.00%

Publicador:

Resumo:

This is a coarse grained sample with some very fine grained domains throughout the sample. The clast shape and size range from small to large, as well as angular to sub-rounded. Grain crushing is the most prevalent in this sample. It also contains some rotation structures and minor necking structures. Lineations and grain stacking can also be seen.