Abstract:The Passa Dois Group is divided into formations and members, representing variations of lithofacies separated by unconformities or correlative conformities.The contact between the Passa Dois and Tubarão Groups is represented by a paraconformity, and the contact between the Passa Dois and São Bento Groups corresponds to a regional unconformity or correlative conformity.Intracratonic basins differ physiographically from passive margin basins, for which the concepts of Sequence Stratigraphy were originally develo… Show more
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