29 resultados para well dispersed clasts

em Brock University, Canada


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Sample contains well dispersed clasts ranging from small to medium in size. They are sub-angular to sub-rounded in shape. Organic rich domains can be seen throughout the sample with clear boundaries. It also contains water escape structures, seen mainly through clay. Lineations are also present.

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This sample contains two different domains; a coarse grained domain with well dispersed clasts, and a fine grained domain that potentially contains organics. The coarser grained domain contains comet structures, lineations and minor rotation without a central grain.

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Brown sediment with well dispersed clasts. Clasts range from small to medium in size and sub-angular to sub-rounded in shape. Alternating domains can be seen (light and dark). Darker domains appear organic rich. Lineations can also be seen throughout the sample.

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Brown sediment with well dispersed clasts. Clasts range from small to medium in size and angular to sub-rounded in shape. Some appear to have been weathered. Water escape structures can be seen, mainly in finer, clay rich sediment. Lineations can also be seen throughout the sample. Minor grain stacking and crushing are also present.

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Dark brown sediment with well dispersed clasts ranging from small to medium in size. Clast shape ranges from sub-angular to sub-rounded. Lineations can commonly be seen throughout the sample. Comet structures can also be seen in minor amounts.

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Dark brown sediment, almost black due to organic material. Mainly structure-less with a few well dispersed clasts. Grains range from small to medium in size and sub-angular to rounded in shape.

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Dark brown sediment with well dispersed clasts. The clasts are mainly small and range from sub-angular to rounded in shape. This sample is mainly structure-less but does contain lineations.

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Dark brown sediment with well dispersed clasts. Clasts are mainly small and range from sub-angular to rounded. Not many structures are present in this sample, aside from some lineations.

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Dark brown sediment with a few well dispersed clasts. Grains are small, and range from angular to sub-rounded. This sample is mainly structure-less with a few lineations.

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This sample contains two main domains. One is a light brown sediment domain with mainly small clasts which are clustered together. Only a few larger clasts can be seen in this domain. The other one is dark brown with well dispersed clasts. The light brown domain contains clasts that range from sub-angular to sub-rounded in shape. Lineations can be commonly seen in this domain. Grain crushing is also common with minor amounts of rotation. In the dark brown domain, clasts range from small to medium in size. They range from sub-angular to sub-rounded in shape. A few lineations and rotation structures can be seen in this domain.

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Brown sediment with well dispersed clasts ranging from small to large. Clast shape ranges from angular to sub-rounded. Lineations can be seen throughout the sample. There is one small patch of another domain present. This domain is light brown, and contains clasts that are clustered together. Grain crushing is abundant in this domain, as well as in other areas of the sample.

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Brown sediment with clasts ranging from small to large in size. Clast shape ranges from sub-angular to sub-rounded. Many grains are fractured throughout the sample. Some lineations can be seen. The sample contains well dispersed clasts.

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Dark brown sediment with well dispersed clasts. The clasts range from small to large in size and sub-angular to sub-rounded in shape. The sample is abundant in rotation structures and lineations. It also contains comet structures and minor amounts of grain stacking.

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This sample contains a fine grained, dark grey ground mass with well dispersed clasts. Clasts are not abundant but range from small to large. The clast shape ranges from sub-angular to sub-rounded. A few faint rotation structures can be seen. Minor amounts of lineations can also be seen.

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Brown sediment with well dispersed clasts ranging from small to large. Clast shape ranges from angular to sub-rounded. Lineations and rotation structures can be seen in this sample. Minor amounts of edge-to-edge grain crushing can also be seen.