A natural salt or mineral deposit left after the evaporation of a body of water.
- Turbidite deposits and westward younging of limestones and evaporites record the development of the foreland fold and thrust belt during the Late Carboniferous Epoch.
- The Rhaetian-Lower Sinemurian shallow ramp units are composed of platform carbonates, evaporites and minor siliciclastic deposits.
- At the same time, lagoonal evaporites were deposited in the middle of the Western Carpathians; therefore an island surrounded by lagoons is hypothesized there.
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