Classification and geodynamic interpretation of hiatuses in the voronezh anteclise

2000 
Hiatuses register, on the one hand, stages of continental development and formation of peneplanation surfaces of different types and ranks, to some of which weathering crusts can be related, and on the other hand, unconformity surfaces dividing a sedimentary cover into structural stages reflecting a cyclic recurrence in the development of a tectonic structure. The hierarchy of hiatuses is correlated with the peculiarities of platformal geodynamics.
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