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最大海泛面

维基百科,自由的百科全书

最大海泛面(英语:Maximum flooding surface)是指海侵最大时所形成的沉积界面,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]。为海侵体系域的顶界面,代表海侵与海退的划分界限。这时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,海域最广最深,陆源物资最远,故沉积速率最低,碎屑颗粒也最细。在岩石露头[2],岩芯及测井曲线[3][4]。可由凝缩层判定,地震剖面上可由最高上超点及其反射面认出[5]

参考文献

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  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