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cementation

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Cementation


The fusion of rock sediments or the remains of microscopic marine organisms into sedimentary rocks. As the material builds up it is compacted together. Cementation occurs as chemical precipitation deposits micro crystals in the spaces between the mineral fragments and grains, holding them together. The ‘cement’ formed may be silica, iron oxide, or carbonate. Cementation contributes to the processes involved in the rock cycle, the formation, change, and reformation of rocks.

Clastic sedimentary rocks, such as sandstone, siltstone, and claystone, are made from the sediments of other rocks. Non-clastic sedimentary rocks, such as limestone and chalk, are of organic origin. Silica cementation takes place below the water table surface; its source is groundwater. Carbonate cementation, also sourced from groundwater, takes place either at above or below ground level. Iron-oxide cementation is less frequent.

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