最大海泛面
外觀
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最大海泛面(英語:Maximum flooding surface)是指海侵最大時所形成的沉積界面,以從退積式准層序組合轉換為加積式或進積式准層序組合為特徵[1]。為海侵體系域的頂界面,代表海侵與海退的劃分界限。這時上覆的高水位體系域的前積層前端下超於最大海泛面之上,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]。可由凝縮層判定,地震剖面上可由最高上超點及其反射面認出[5]。
參考文獻
[編輯]- ^ Catuneanu, Octavian (2011). "Sequence stratigraphy: methodology and nomenclature". Newsletters on Stratigraphy. E. Schweizerbart'sche Verlagsbuchhandlung.44(3): 190
- ^ 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
- ^ 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
- ^ 宋子齊等人,2009. 利用自然電位與自然伽馬測井曲線劃分沉積相帶及儲層分佈。地球物理學進展 Vol. 24 ›› Issue (2): 651-656.doi: 10.3969/ j.issn.1004-2903.2009.02.038
- ^ Van Wagoner, J.C., 1988. AN OVERVIEW OF THE FUNDAMENTALS OF SEQUENCE STRATIGRAPHY AND KEY DEFINITIONS.SEPM Special Publication ISBN 0-918985-74-9