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- Clastic_dike abstract "A clastic dike is a seam of sedimentary material that fills a crack in and cuts across sedimentary strata or other rock types. Clastic dikes form rapidly by fluidized injection (mobilization of pressurized pore fluids) or passively by water, wind, and gravity (sediment swept into open cracks). Diagenesis may play a role in the formation of some dikes. Clastic dikes are commonly vertical or near-vertical. Centimeter-scale widths are common, but thicknesses range from millimetres to metres. Length is usually many times width.With phrasing typical of the early-century American geologist, Olaf P. Jenkins states, "It appears, then, that in every case fissures formed and then fragmental materials are dropped, washed, or pressed into them, from above, below, or from the sides. This action has taken place in open fissures; under water in fissures on the bed of the sea or other bodes of water; and also far below the surface of the earth in consolidated rocks. The filling from below has come about by pressure of some sort, in some cases undoubtedly hydrostatic."Clastic dikes are found in sedimentary basin deposits worldwide. Formal geologic reports of clastic dikes began to emerge in the early 19th century.Terms synonymous with clastic dike include: clastic intrusion, sandstone dike, fissure fill, soft-sediment deformation, fluid escape structure, seismite, injectite, liquefaction feature, neptunian dike, paleoseismic indicator, pseudo ice wedge cast, sedimentary insertion, sheeted clastic dike, synsedimentary filling, tension fracture, hydraulic injection dike, and tempestite.".
- Clastic_dike thumbnail Coarse_sand_dike_Starbuck.JPG?width=300.
- Clastic_dike wikiPageID "7144452".
- Clastic_dike wikiPageRevisionID "573606599".
- Clastic_dike hasPhotoCollection Clastic_dike.
- Clastic_dike subject Category:Sedimentary_rocks.
- Clastic_dike type Abstraction100002137.
- Clastic_dike type Material114580897.
- Clastic_dike type Matter100020827.
- Clastic_dike type Part113809207.
- Clastic_dike type PhysicalEntity100001930.
- Clastic_dike type Relation100031921.
- Clastic_dike type Rock114696793.
- Clastic_dike type SedimentaryRock114698000.
- Clastic_dike type SedimentaryRocks.
- Clastic_dike type Substance100019613.
- Clastic_dike comment "A clastic dike is a seam of sedimentary material that fills a crack in and cuts across sedimentary strata or other rock types. Clastic dikes form rapidly by fluidized injection (mobilization of pressurized pore fluids) or passively by water, wind, and gravity (sediment swept into open cracks). Diagenesis may play a role in the formation of some dikes. Clastic dikes are commonly vertical or near-vertical. Centimeter-scale widths are common, but thicknesses range from millimetres to metres.".
- Clastic_dike label "Clastic dike".
- Clastic_dike label "Neptunian Dike".
- Clastic_dike label "Żyła klastyczna".
- Clastic_dike sameAs Neptunian_Dike.
- Clastic_dike sameAs Żyła_klastyczna.
- Clastic_dike sameAs m.0h6kym.
- Clastic_dike sameAs Q1977889.
- Clastic_dike sameAs Q1977889.
- Clastic_dike sameAs Clastic_dike.
- Clastic_dike wasDerivedFrom Clastic_dike?oldid=573606599.
- Clastic_dike depiction Coarse_sand_dike_Starbuck.JPG.
- Clastic_dike isPrimaryTopicOf Clastic_dike.
