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Assise
An assise (from the Fr., derived from Latin ''assidere'', "to sit beside"), is a geological term for two or more beds or strata of rock united by the occurrence of the same characteristic species or genera. In the hierarchy of stratigraphic units, an assise lies between a stage (or sub-stage) and a stratum. ==References==
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抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Assise」の詳細全文を読む
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