Transgressive facies sequence of a high energy, wave-tide-storm-influenced shoreface: A case study of the east Frisian Barrier Islands (Southern North Sea)

Author:

Antia Effiom,Flemming Burghard,Wefer Gerold

Publisher

Springer Science and Business Media LLC

Subject

Paleontology,Stratigraphy,Geology

Reference37 articles.

1. Aigner, T. A. &Reineck, H.-E. (1982): Proximality trends in modern storm sands from the Helgoland Bight (North Sea) and their implications for basin analysis.—Senckenbergiana marit.,14, 183–215, Frankfurt a.M.

2. — &— (1983): Seasonal variation of wave-base on the shoreface of the barrier island Norderney, North Sea.—Senckenbergiana marit.,15, 87–92, Frankfurt a.M.

3. Anderton, R. (1976): Tidal-shelf sedimentation: an example from the Scottish Dalradian.—Sedimentology,23, 429–458, Oxford

4. Antia, E. E. (1992): Sedimentology, morphodynamics and facies association of a mesotidal barrier island shoreface, Spiekeroog, southern North Sea.—Ph.D Thesis, Geological Sciences Institute, Univ. Bremen, 370 p., Bremen

5. — (1993): Surficial grain-size statistical parameters of a North Sea shoreface-connected ridge: patterns and process implication.—Geo-Mar. Letters,13, 172–181, Berlin

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