Einsele et al (1991) note that
processes that are influenced by events external to the depositional basin
including climate, tectonic movement and eustasy primarily control these
sequences. Beds of these cyclic sequences have often have widespread continuity
with the processes involved having operated in several adjacent or widespread
basins. Examples may include the sequences of Vail et al 1971.
References
Dott R.H. 1988, An episodic
view of shallow marine clastic sedimentation. In de Boer P. L. van Gelder
A., Nio S.D. eds Tide influenced sedimentary environments and facies.
Reidel , Dordecht, pp3-12
Einsele
G., Ricken W., and Seilacher A., (editors), 1991, "Cycles and
events in stratigraphy", Springer-Verlag, Berlin, Heidelberg, New
York 1991. 955p.
Vail, P. R. , R. G. Todd,and J. B. Sangree, 1977, Seismic Stratigraphy and Global Changes of Sea Level: Part 5. Chronostratigraphic Significance of Seismic Reflections: Section 2. Application of Seismic Reflection Configuration to Stratigraphic Interpretation Memoir 26, Pages 99 – 116.
