| 层序：一个新地层单位的自述 |
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| 引用本文： | 陈中强.层序：一个新地层单位的自述[J].地层学杂志,1995,19(4):274-281. |
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| 作者姓名： | 陈中强 |
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| 作者单位： | 中国科学院南京地质古生物研究所 |
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| 摘 要： | 层序是层序地层学常用的且最重要的地层单位，它既是以客观不整合面为界面的岩石地层单位，又是有严格时间属性的年代地层单位，具岩石地层单位和年代地层单位的两重性，它具横向可预测、全盆地统一及时限短等特性。与传统的地层单位有严格的区别，克服了岩石地层、生物地层及年代地层在划分与对比地层时的缺点，提高了地层划分与对比的精度。
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| 关 键 词： | 层序，岩石地层单位，年代地层单位，层序地层单位体系 |
Sequence: a new stratigraphic unit |
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| Chen Zhongqiang.Sequence: a new stratigraphic unit[J].Journal of Stratigraphy,1995,19(4):274-281. |
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| Authors: | Chen Zhongqiang |
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| Abstract: | Sequence is the commonest and most important sequence stratigraphic unit.It is characterized by the features of both lithostratigraphic unit bounded by objective unconformity and chronostratigraphic unit marked by strict property of time.In addition,sequence is also characterized by the features of the lateral forcasting,basinwide unify and limited time line. It is different with the traditional stratigraphic unit. |
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| Keywords: | sequence lithostratigraphic unit chronostratigraphic unit sequence stratigraphic unit system |
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