F. Robaszynski
University of Nottingham
8 Papers
102 Citations
F. Robaszynski is an academic researcher from University of Nottingham. The author has contributed to research in topics: Cenomanian & Cretaceous. The author has an hindex of 7, co-authored 8 publications. Previous affiliations of F. Robaszynski include Faculté polytechnique de Mons.
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Papers
The cretaceous of the boulonnais (France) and a comparison with the cretaceous of Kent (United Kingdom)
F. Robaszynski,F. Robaszynski,Francis Amédro,Francis Amédro +3 more
- 01 Jan 1986
TL;DR: The distribution, structure and stratigraphy of the Boulonnais Cretaceous is summarised, followed by a more detailed discussion of representative sections of the Wealden, Aptian, Albian and Chalk.
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La géochimie isotopique du carbone (δ13C) comme outil stratigraphique. Application à la limite Cénomanien/Turonien en Tunisie centrale
H. Accarie,Laurent Emmanuel,F. Robaszynski,François Baudin,Francis Amédro,Michèle Caron,J.-F. Deconinck +6 more
- 01 Jan 1996
TL;DR: The carbon isotope profile (δ 13 C) around the Cenomanian/Turonian boundary is defined in central Tunisia on a section which is dated by ammonites as discussed by the authors.
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The Cenomanian-Turonian boundary in central Tunisia in the context of a sequence-stratigraphic interpretation
TL;DR: A preliminary evaluation of the position of the depositional sequences in the middle and upper Cenomanian relative to the standard ammonite zones shows a sequence boundary in the upper part of the middle cenomanians and one in the Upper Cenominians as discussed by the authors.
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La limite Cénomanien-Turonien et la Formation Bahloul dans quelques localités de Tunisie Centrale
TL;DR: The Bahloul Formation as discussed by the authors has been shown to have developed during the latest Cenomanian by ammonite records and it is demonstrated on the basis of ammonite recordings that the main part of the Bahoul facies developed in the earliest Turonian north-east of Jerissa.
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Niveaux reperes de bentonite d'origine volcanique dans les craies du turonien du boulonnais et de haute-normandie
J.-F. Deconinck,F. Amedro,A. Desprairies,P. Juignet,F. Robaszynski +4 more
- 01 Jan 1991
TL;DR: The clay assemblages of marly levels identified in Upper Turonian chalk in the Boulonnais and Normandy are composed almost entirely of magnesium-rich dioctahedral smectite resulting from submarine alteration of volcanic glass shards as discussed by the authors.
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