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Erathem

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erathem [′erĀ·ə‚them]
(geology)
A chronostratigraphic unit, below eonothem and above system, composed of rocks formed during an era of geologic time.

Erathem 

(geology), a subdivision of the general stratigraphic scale, subordinate to the eonothem and itself subdivided into stratigraphic systems. In the Russian geological literature, the erathem was usually called group. In 1966, the American geologist H. Hedberg suggested the term “erathem,” which was adopted in the USSR in 1976. The time interval during which an erathem forms corresponds to an era. (See alsoSTRATIGRAPHY.)



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Hence, we can refer to the Maastrichtian Stage of the Cretaceous System of the Mesozoic Erathem in a chronostratigraphic sense or to the Maastrichtian Age of the Cretaceous Period of the Mesozoic Era in a geochronologic sense; similarly, chronostratigraphic units can be subdivided into lower, middle and upper subunits; geochronologic units can be subdivided into early, mid and late subunits.
 
 
 
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