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Relationship between sequence stratigraphical boundary and chronostratigraphical boundary

机译:层序地层界线与年代地层界线的关系

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Sequence stratigraphy is a science studying the genetically related facies within a chronostratigraphic framework. Sequence is the basic unit of sequence stratigraphy, which is a "succession of genetically related, essentially conformable strata bounded below and above by unconformities and their correlative conformities. Sequence boundaries with uncomformity surface on shelf and correlative conformity surface in basin are defined as synchronous, and thus have chronostratigraphic implication. As a result, there should be certain intrinsic relation between the basic units of sequence stratigraphy and chronostratigraphy. To make clear the intrinsic relation between these two stratigraphic units and to improve the methodology of chronostratigraphic subdivision such as stage are an important task in the study of stratigraphy.
机译:层序地层学是一门研究年代地层学框架内与遗传有关的相的科学。层序是层序地层学的基本单位,它是“由不整合面及其相关整合面上下限定的遗传相关,基本整合层的继承。架子上不整合面和盆地相关整合面的层序边界被定义为同步,因此,层序地层学和年代地层学的基本单元之间应该有一定的内在联系,以弄清这两个地层学单元之间的内在联系,并改善年代地层划分的方法论,例如阶段性。在地层学研究中的重要任务。

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