Condensation and channelling in Cenomanian chalks of the northern Anglo-Paris Basin; The Totternhoe Stone and related deposits

Author(s):  
Andy Gale ◽  
Jim Kennedy
Keyword(s):  
1948 ◽  
Vol S5-XVIII (6-7) ◽  
pp. 565-574 ◽  
Author(s):  
Andre Chavan
Keyword(s):  
The West ◽  

Abstract Concludes that the pisolitic limestone overlying Campanian and in places Maestrichtian (Cretaceous) formations of the Paris basin, France, was formed during at least two stages and should be qualified as a Dano-Montian formation. Transgression of the sea was both from the northeast and, in the later stage, from the west, which accounts for the mixed fauna.


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