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Revision 5181913 of "Litostratigrafia" on skwiki

{{urgentne upraviť|20130215}}
Vychádza priamo z horninového charakteru vrstiev. Jej účelom je presné usporiadanie vrstvových komplexov do pomenovaných jednotiek, ktoré zastupujú základné zmeny charakteru ich hornín.
Základnou litostaratigrafickou jednotkou je súvrstvie(formation), ktorá sa člení na litologicky odlišné členy(member). Litologicky výrazne jednotná, najmenšia formálna jednotka je vrstva(bed).

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