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In the lithification process, compaction is followed by cementation. It is the hardening and welding of clastic sediments by the precipitation of mineral matter.
Lithification involves the compaction and cementation of sediment into rock.
compaction and cementation
Compaction is a step in the creation of detrital sedimentary rock, those formed from the lithification of sediments.
Lithification refers to the process in which sediments compact under pressure. The two primary agents of lithification are compaction and cementation.
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Because sands and other coarse sediments are less compressible, compaction is most significant as a lithification process in fine-grained sedimentary rock.
Lithification processes, collectively referred to as "diagenesis," include: compaction (example: clay to shale), cementation (example: sand to sandstone), and partial recrystallization (example: lime mud to limestone). Note: Pressure by itself does not by compaction lithify sand to sandstone. Sandstone diagenesis is mostly by cementation and also, sometimes, by partial recrystallization and crystal overgrowths. The same is so of gravel that lithifies to conglomerate.
The type of sediment that undergoes the most compaction as it lithifies to sedimentary rocks is marine mud. Lithification refers to the process wherein sediments compact under pressure.
Lithification
In the lithification process, compaction is followed by cementation. It is the hardening and welding of clastic sediments by the precipitation of mineral matter.
Lithification involves the compaction and cementation of sediment into rock.
compaction and cementation
compaction and cementation
Cementation.
Lithification is the compaction of materials into a sedimentary rock, such as sandstone.
compaction and cementation.