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顶超

维基百科，自由的百科全书

顶超（英语：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，每一倾斜地层的尖灭点往盆地方向超越早一倾斜地层的尖灭点，是海平面相对静止的标志。[1][2][3]

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参考资料

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  1. ^ R. M. Mitchum Jr 1977 Seismic Stratigraphy and Global Changes of Sea Level: Part 11. Glossary of Terms used in Seismic Stratigraphy: Section 2. Application of Seismic Reflection Configuration to Stratigraphic Interpretation， in AAPG Memoir 26: Seismic Stratigraphy--Applications to Hydrocarbon Exploration
  2. ^ Stokes, W. Lee (1982).Essentials of Earth History 4th Edition. Prentice Hall,Inc.ISBN 0-13-285890-8
  3. ^ Monroe J.S., Wicander R. & Hazlett R.W. (2007).Physical geology: exploring the Earth. Cengage Learning.ISBN 9780495011484
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