Results 1 to 10 of about 19 (10)
Support for a Vraconnian Stage between the Albian sensu stricto and the Cenomanian (Cretaceous System) [PDF]
Carnets de Géologie, 2008 The geological scale for the middle Cretaceous currently used throughout the world was proposed by Alcide d'Orbigny in the XIXth century between the years 1842 and 1847 and establishes the succession of stages as Albian, Cenomanian and Turonian.
Amédro Francis
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Zonation by ammonites and foraminifers of the Vraconnian-Turonian interval: A comparison of the Boreal and Tethyan domains (NW Europe / Central Tunisia) [PDF]
Carnets de Géologie, 2008 Since the end of the 19th century the interval comprising the uppermost Upper Albian, the Cenomamian, the Turonian and the basal Coniacian has been subdivided, first into ammonite zones, then, beginning in the middle of the 20th century, into zones of ...
Amédro Francis, Robaszynski Francis
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Bulletin de la Société Géologique de France, 2008 AbstractThrough the description and interpretation of the position of macro- and microfossils in several sections of the Albian-Cenomanian boundary in SE France and Central Tunisia, a comparison is made between the north and south margins of the Tethyan Ocean by using the occurrences of marker bioevents.
Robaszynski, Francis +3 more
openaire +3 more sources
Uppermost Albian biostratigraphy and chronostratigraphy
Carnets de Géologie, 2009 The Albian Stage is the highest chronostratigraphic unit of the Lower Cretaceous Series and underlies the Cenomanian Stage of the Upper Cretaceous Series.
Scott Robert W.
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Carnets de Géologie, 2009 Because of urbanization the section at Gargas, historical stratotype of the Aptian stage and of the Gargasian substage, is no longer accessible. However, samples taken there in 1966 by one of us make feasible a reinterpretation of this series in the ...
Moullade Michel +2 more
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The Gargasian of Gargas (Vaucluse, SE France) : Synthesis of field data and revision of the foraminiferal and ostracodal microfauna [PDF]
, 2009 Because of urbanization the section at Gargas, historical stratotype of the Aptian stage and of the Gargasian substage, is no longer accessible. However, samples taken there in 1966 by one of us make feasible a reinterpretation of this series in the ...
Babinot, Jean-François +5 more
core +1 more source
, 2000 The Marcoule silty shales Formation of the ANDRA borings In the rhodanian Gard (SE France) : the uppermost Albian ("Vraconnian")-Cenomanian boundary by means of ammonites. Comparison with the Salazac outcrops. In the rhodanian part of the Gard department
Amédro, Francis, Robaszynski, Francis
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, 2017 Lithostratigraphical analysis of more than ten sections of the El Mizab Formation (Talerhza Basin), previously assigned to the "Vraconnian" lead to distinguish a similar succession of five members, called from oldest to youngest: Silty marly limestones ...
Oumhamed, Mohamed +3 more
core +1 more source
Relations between the northern and southern margins of the Tethys ocean during the Cretaceous period
Carnets de Géologie, 2007 A set of 11 abstracts and short papers (extended abstracts) of presentations given at a meeting organized by the "Groupe Français du Crétacé (GFC)", held on November 27-28, 2007 at the "École des Mines" in Paris ...
Bulot Luc G. +2 more
doaj
, 2007 International audienceLes bioévénements de la limite Albien (Vraconnien) - Cénomanien aux marges nord et sud de la Téthys (S.E. de la France et Tunisie centrale) [Bioevents at the Albian (Vraconnian) - Cenomanian boundary at the North and South margins ...
Amédro, Francis +3 more
core