Evidence of Tectonic Control on the Geochemical Features of the Volatiles Vented along the Nebrodi-Peloritani Mts (Southern Apennine Chain, Italy)

<div>CH<sub>4</sub>-O<sub>2</sub>-CO<sub>2</sub> composition of the gases dissolved in the studied waters. The dashed arrows show the trends produced by the addition and dissolution of CO<sub>2</sub> and addition of CH<sub>4</sub> to an atmospheric gas assemblage (see text for details). ASW: air saturated water. Open black marks: samples from Nebrodi Mts; blue filled marks: samples from Peloritani Mts. Labels refer to sample numbers as in Tables <a href="../tab1/">1</a>–<a href="../tab4/">4</a>.</div>

Geofluids

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Figure 2

Figure 2: Evidence of Tectonic Control on the Geochemical Features of the Volatiles Vented along the Nebrodi-Peloritani Mts (Southern Apennine Chain, Italy) 

Figure 2 | Evidence of Tectonic Control on the Geochemical Features of the Volatiles Vented along the Nebrodi-Peloritani Mts (Southern Apennine Chain, Italy) 