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Siltstone

Aleurite ( English aleurite, silt ; German Aleurit ; from other Greek. Ἄλευρον “flour”) is a loose finely clastic sedimentary rock .

Description

Aleurite consists mainly of mineral grains ( quartz , feldspars , mica, and others) of 0.01-0.1 mm in size, occupying an intermediate position between clay and sand ( loess , silt , dust ).

According to the prevailing grains, large-aleurite (0.05-0.1 mm) and fine-aleurite or fine aleurite (0.01-0.05 mm) varieties of aleurite are distinguished.

Aleurite was separated into a separate sedimentary rock at the proposal of the Soviet petrograph A.N. Zavaritsky in 1930.

Aleurite is used in the manufacture of cement.

As a result of lithification, silt turns into siltstone .

Literature

  • "Geological Dictionary", M: "bowels", 1978.

Links

  • Aleurite // Great Soviet Encyclopedia : [in 30 vol.] / Ch. ed. A.M. Prokhorov . - 3rd ed. - M .: Soviet Encyclopedia, 1969-1978.
  • Aleurite - article from the Great Encyclopedia of Cyril and Methodius



Clastic rocks
Breed groupDebris sizeincoherentCemented
RoundedNeokatannyeRoundedthe sharp-edged
Coarse rocks ( psephitis )10 - 1 mBlock boulderslumps--
1 m - 10 cmbouldersBreaks (blocks)Boulder conglomerateOtlomovaya (bloc) breccias
10 - 1 cmpebblecrushed stonePebble conglomeratesCrushed Breccias
1 cm - 2 mmGravelDresvaGravelitesGingerbread man
Sand rocks ( psammity )2 - 0.05 mmSandsSandstones
Silty rocks ( siltstones )0.05 - 0.005 mmSiltstoneSiltstone
Argillaceous rocks ( pelites )<0.005 mmSilt , clayClays , mudstones
Source - https://ru.wikipedia.org/w/index.php?title=Aleurit&oldid=85194637


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