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. 2014 Aug 12;15:12. doi: 10.1186/s12932-014-0012-y

Figure 13.

Figure 13

δ 34 S SO4 values exhibit an inverse relationship with chloride concentrations. A conservative mixing model demonstrates elevated contributions of high-Cl fluid in Rocky Point (●), Spiegelei (▲), and the Brine pool (×), relative to Twinkie (+), background sediments (◇), and surface seawater (■).