最大海泛面

最大海泛面（英語：）是指海侵最大时所形成的沉積界面，以从退积式准层序组合转换为加积式或进积式准层序组合为特征[1]。為海侵体系域的顶界面，代表海侵與海退的劃分界限。這時上覆的高水位体系域的前积层前端下超于最大海泛面之上，海域最廣最深，陸源物資最遠，故沉積速率最低，碎屑顆粒也最細。在岩石露頭[2]，岩芯及測井曲綫[3][4]。可由凝缩层判定，地震剖面上可由最高上超點及其反射面認出[5]。

參考文獻
  1. Catuneanu, Octavian (2011). "Sequence stratigraphy: methodology and nomenclature". Newsletters on Stratigraphy. E. Schweizerbart'sche Verlagsbuchhandlung.44(3): 190
  2. Monroe, J. S., and Wicander. R. 1997.The Changing Earth: Exploring Geology and Evolution, 2nd ed. Belmont: West Publishing Company, 1997, pp. 112 - 113 ISBN 0-314-09577-2
  3. Oresajo, B., et al. 2015.Sequence stratigraphy and structural analysis of the Emi field offshore depobelt, Eastern Niger Delta Basin, Nigeria. 2015, Ife Journal of Science, vol. 17
  4. 宋子齐等人，2009. 利用自然电位与自然伽马测井曲线划分沉积相带及储层分布。地球物理学进展 Vol. 24 ›› Issue (2): 651-656.doi: 10.3969/ j.issn.1004-2903.2009.02.038
  5. Van Wagoner, J.C., 1988. AN OVERVIEW OF THE FUNDAMENTALS OF SEQUENCE STRATIGRAPHY AND KEY DEFINITIONS.SEPM Special Publication ISBN 0-918985-74-9
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