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陆相地层的层序地层学:层序的特征与模式
引用本文:刘立,王东坡.陆相地层的层序地层学:层序的特征与模式[J].沉积与特提斯地质,1996,16(5):47-53.
作者姓名:刘立  王东坡
作者单位:长春地质学院
摘    要:陆相地层的层序地层学研究近年来取得了较大的进展,尤其在层序的组成、层序界线和最大洪泛面的识别以及层序模式的建立等方面研究得比较深入。层序地层的组成包括层序组合和层序的内部单元。层序界线和最大洪泛面的识别是陆相地层层序地层学研究的关键。目前已初步建立了箕状断陷盆地、坳陷盆地以及冲积地层背景的层序模式。

关 键 词:陆相地层层序地层学,层序地层的组成,层序界线,最大洪泛面,层序模式
收稿时间:1995/4/23 0:00:00

SEQUENCE STRATIGRAPHY OF CONTINENTAL STRATA: CHARACTERISTICS AND MODELS
Liu Li,Wang Dongpo.SEQUENCE STRATIGRAPHY OF CONTINENTAL STRATA: CHARACTERISTICS AND MODELS[J].Sedimentary Geology and Tethyan Geology,1996,16(5):47-53.
Authors:Liu Li  Wang Dongpo
Institution:Changchun University of Earth Sciences
Abstract:The last few years has seen a considerable advance in sequence stratigraphy of continental strata, especially in the studies of sequence stratigraphic units, recognition of sequence boundaries and maximum flooding surfaces,and sequence models.The sequence stratigraphic units include the associations and internal units of the sequences. The recognition of sequence boundaries and maximum flooding surfaces is the key problem in the study of sequence stratigraphy of continental strata. The sequence models for a half graben-like fault basin, downwarped basin and alluvial strata have also been constructed in this paper.
Keywords:sequence stratigraphy of continental strata  sequence stratigraphic unit  sequence boundary  maximum flooding surface  sequence model  
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