The unconformity, river rejuvenation surface and lithology and lithofacies transition surface are the main types of sequence boundaries.
层序界面类型主要有不整合面、河流冲刷侵蚀作用面和岩性岩相转换面等。
The sequence boundaries and the slope-break zones are the important factors to control creation of stratigraphic and lithologic traps in the area.
层序地层边界和坡折带是控制本区地层岩性圈闭形成的重要因素。
The recognition of sequence boundaries and maximum flooding surfaces is the key problem in the study of sequence stratigraphy of continental strata.
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。
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