917 resultados para STACKING-FAULTS


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Brown and coarse grained sample with grains ranging from small to large in size. The clast shape ranges from sub-angular to sub-rounded. Lineations are abundant throughout the sample. Minor amounts of grain crushing/stacking can also be seen. A few rotation structures are also present throughout the sample.

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Mainly a coarse brown sediment with a few patches of a finer grained domain. The clasts range from small to large in size and angular to sub-rounded in clast shape. The coarser domain mainly contains grain crushing and stacking, with some rotation structures. The finer domain mainly contains lineations.

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Brown sediment with grains ranging from small to medium in size. The sample mainly contains smaller clasts. Clast shape ranges from sub-angular to sub-rounded. Water escape structures and lineations can be seen in this sample. Grains stacking and comet structures are also present in minor amounts.

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Brown sediment with clasts that range from small to medium in size. The grain shape ranges from angular to sub-rounded. Lineations and rotation structures were the most common throughout the sample. Grain crushing/stacking and a few comet structures were also present. Clay material was also dispersed throughout the sample.

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Brown sediment with areas of clay rich material (darker brown). Clasts range from small to large in size. Clast shape ranges from angular to rounded. Rotation structures and necking structures were abundant in this sample. Some lineations and grain stacking can also be seen throughout the sample.

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Dark brown sediment with clasts ranging from small to medium in size. The clast shape ranges from angular to sub-rounded. Lineations are abundant throughout the sample. Comet structures and grain crushing/stacking are also present in minor amounts.

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Dark brown sediment with clasts ranging from small to medium in size. The clast shape ranges from angular to sub-rounded. Lineations are commonly seen throughout the sample. Grain crushing/stacking can also be seen along with varying amounts of rotation structures and comet structures.

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Dark brown sediment with clasts ranging from small to medium in size. Clast shape ranges from angular to sub-rounded. Rotation structures and lineations are common throughout the sample. Comet structures and grain stacking/crushing can also be seen in minor amounts.

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Brown sediment with clasts ranging from small to medium in size. The clast shape ranges from angular to sub-rounded. Comet structures, rotation structures, and lineations can be seen throughout the sample. Minor amounts of grain stacking can also be seen.

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Dark brown sediment with clasts ranging from small to medium. The clast shape ranges from angular to sub-rounded. Edge-to-edge grain crushing and grain stacking are abundant throughout this sample. Some lineations and rotation structures can also be seen in minor amounts.

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Brown sediment with clasts ranging from small to medium in size. Clast shape ranges from angular to sub-rounded in shape. Lineations and rotation structures can be seen throughout the sample. Some comet structures and grain stacking can also be seen.

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Brown sediment with organic matter present throughout. Clasts range from small to medium in size and angular to sub-rounded in shape. Lineations are common throughout the sample, with some grain stacking and minor amounts of rotation.

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Brown sediment with clasts ranging from small to medium in size. Clast shape ranges from angular to sub-rounded. Lineations are abundant throughout the sample. Grain crushing, grain stacking and minor amounts of rotation are also present throughout.

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Dark brown sediment with organic matter. There are two main domains; a coarse grained domain, and a finer grained domain. The coarse grained domain contains grains ranging from small to medium in size, and angular to sub-rounded in shape. In the coarse grained domain, grain crushing/stacking is common, with a few lineations and rotation structures. In the finer grained domain, grains are small and range from sub-angular to sub-rounded in shape. Lineations are abundant in this domain.

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Light brown sediment with clasts ranging from small to medium in size. The clast shape ranges from sub-angular to rounded. Lineations and edge-to-edge grain crushing can mainly be seen in this sample. There are also a few examples of grain stacking and crushed grains.