Three litoestratigraphical formations form the Calderona Group, with them the detritic deposits of the upper Permian and lower Triasic are designated for the Espadán-Calderona domain. The series begins with a posthercinic conglomerate. The sedimentary rupture that indicates the basal conglomerate of the second formation (Garbí Sandstone Fm.) could be associated to magmatic processes.
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