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Onlap or overlap is the geological phenomenon of successively wedge-shaped younger rock strata extending progressively further across an erosion surface cut in older rocks. It is generally associated with a marine transgression. It is a more general term than overstep, in which the younger beds overlap onto successively older beds. The opposite is offlap, in which each younger rock bed pinches out short of the full extent of the underlying older bed, typically due to a marine regression.

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  • Onlap (en)
  • 顶超 (zh)
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  • Onlap or overlap is the geological phenomenon of successively wedge-shaped younger rock strata extending progressively further across an erosion surface cut in older rocks. It is generally associated with a marine transgression. It is a more general term than overstep, in which the younger beds overlap onto successively older beds. The opposite is offlap, in which each younger rock bed pinches out short of the full extent of the underlying older bed, typically due to a marine regression. (en)
  • 顶超(英語:toplap)是层序顶界的超失,一系列低角度倾斜的地层依次终止于水平或更小倾角的顶界面,每一傾斜地層的尖滅點往盆地方向超越早一傾斜地層的尖滅點,是海平面相对静止的标志。 (zh)
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  • Onlap or overlap is the geological phenomenon of successively wedge-shaped younger rock strata extending progressively further across an erosion surface cut in older rocks. It is generally associated with a marine transgression. It is a more general term than overstep, in which the younger beds overlap onto successively older beds. The opposite is offlap, in which each younger rock bed pinches out short of the full extent of the underlying older bed, typically due to a marine regression. (en)
  • 顶超(英語:toplap)是层序顶界的超失,一系列低角度倾斜的地层依次终止于水平或更小倾角的顶界面,每一傾斜地層的尖滅點往盆地方向超越早一傾斜地層的尖滅點,是海平面相对静止的标志。 (zh)
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