The Scythian to HeUangian sedimentary record of the Eastern Spain includes an initial rift-type supersequence (Buntsandstein) and four Depositional Sequences (Muschelkalk-Keuper). Within the rift tectofacies the tectonic influence just charactize a continuous fining-upwards sequence, while in the carbonate ramp and flood plain facies present within the other four Depositional Sequences, TST's and HST's can be differentiated and correlated
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