Abstract
ESR parameters were measured for the CERI- 1 stratigraphic column of the Irati Formation (Parana Basin, Brazil), in order to verify the “anomalous behaviour of the stratigraphic function of paleotemperature” observed for the same column by Costa Neto et al. (1978) and contradicted by Correa da Silva and Conford (1985). The good correlation observed between stratigraphic functions of ESR and of thermal alteration index (TAI) confirms the results reported by Costa Neto et al. (1978).
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