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Coupled measurements of δ18O and δD of hydration water and salinity of fluid inclusions in gypsum from the Messinian Yesares Member, Sorbas Basin (SE Spain)

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Academic year: 2020

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Figure

Fig. 1. (A) Location map of the Sorbas Basin and surrounding areas modified after Krijgsman et al
Fig. 2. Cycle 6 of the Río de Aguas section, displaying the differing crystal morphology and structures (A) relative to a schematic diagram (B) (after Dronkert, 1977)
Fig. 3. δ34S vs. δ18O of sulfate of the Yesares Gypsum. Messinian seawater values of ∼22.5h and ∼13.5h for δ34S and δ18OSO4 , respectively (Paytan, 1998; Turchyn and Schrag, 2004), are marked with star.
Fig. 5. (A) The ratio of dolomite to calcite of the marls at the base of the section. % gypsum is obtained from XRD data; (B) δ18Ocarb, δ13C and % dolomite in the marls at the base of the section
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