Notable Examples of Thick Evaporites in Geological Basins

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Evaporites form when dissolved salts precipitate out of sea water due to concentration during distillation.

False

Sea water typically contains 35 grams per liter of dissolved ions.

True

The least soluble compounds precipitate last during the formation of evaporites.

False

Temperature has no effect on the amount of ions precipitated during the formation of evaporites.

False

Calcium sulphate can precipitate as gypsum or anhydrite during the evaporite formation process.

True

Gypsum and anhydrite are the most commonly encountered evaporite minerals in sedimentary rocks.

True

Evaporites are formed from the precipitation of minerals dissolved in water

True

The evaporites in the Michigan Basin are thicker than those in the Messinian of the Mediterranean basin

False

Gypsum and anhydrite are examples of irreversible reactions in evaporite formation

False

Evaporites are commonly found in marine basin settings due to the high evaporation rates

True

The Upper Silurian evaporites of the Michigan Basin are older than the Messinian evaporites of the Mediterranean basin

False

Evaporites are commonly found only in marine environments.

False

Gypsen and anhydrite are examples of evaporite minerals.

True

Evaporite minerals like gypsen can act as cap rocks to carbonate reservoir rocks.

True

Salt diapirism is a process involving the formation of gypsen.

False

Reversible reactions can convert anhydrite into gypsum under certain conditions.

True

Learn about two notable examples of thick evaporites found in geological basins: the >2-km-thick evaporites of the Messinian (Miocene) in the Mediterranean basin and the >600-m-thick Upper Silurian evaporites in the Michigan Basin.

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