SULFATEISOTOPECOMPOSITIONS (δ 34 S, δ 18 O) AND STRONTIUM ISOTOPIC RATIOS ( 87 Sr/ 86 Sr) OF TRIASSIC EVAPORITES IN THE BETIC

Sulfate isotope compositions (δ 34 S and δ 18 O) and strontium isotope ratios ( 87 Sr/ 86 Sr) of Tri- assic evaporites in the Betic Cordillera are addressed for the first time in the present work. Isotope val- ues have been determined in gypsum and anhydrite samples of the Germanic-type facies (Buntsandstein, Muschelkalk and Keuper) coming from different outcrops spanning the complete Triassic Period and cor - responding to both the Internal Zones and the External (Prebetic, Subbetic) Zones of this chain. More precise age assignments and stratigraphic controls are often obscured because of the intense halokinetic and tectonic deformation occurred during the Alpine Orogeny in the Betic Cordillera. Isotope values of Triassic sulfates obtained in the present study range between 12.5 and 16.6 ‰ for δ 34 S, between 8.9 and 16.9 ‰ for δ 18 O, and between 0.707615 and 0.708114 for 87 Sr/ 86 Sr. These values, as a whole, are in