Paleoceanographic conditions which led to the formation of the
"mid"-cretaceous triad along the northern Tethys margin are
elucidated. In the first part, the evolution of this sequence is
traced from the demise of the platform to the return of the
detritus dominated deposition. The second part includes a
discussion of the reconstructed paleoceanographic and tectonic
variables, their possible interaction as well as their influence on
sediment properties.
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