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Toe-of-slope megabreccia deposits of an Upper Cretaceous rudist platform were studied in the Bakony Mountains. During the Turonian-early Senonian tectogenesis an articulated basin came into being in the area of the Bakony; depressions and highs were formed roughly parallel with the structural strike of the mountains. Inundation of the highs led to the evolution of carbonate platforms. The investigated...
Oxfordian and Berriasian sections representing shallow-water, carbonate-dominated sedimentary systems have been studied in the Swiss and French Jura, in Spain, and in Normandy. They all display a hierarchical stacking of depositional sequences. Facies evolution and stacking pattern allow to define elementary, small-scale, medium-scale, and large-scale sequences. Some depositional sequences display...
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