Table 1 Mixing model parameters.

From: Deep submarine infiltration of altered geothermal groundwater on the south Chilean Margin

 

Cl

Na+

K+

DSi

Ca2+

Mg2+

δ18O

δD

87Sr/86Sr

SW

544 mM

470 mM

10 mM

24 µM

10 mM

54 mM

−0.159 ‰

−1.7 ‰

0.7092

GT

18.5 ± 12.4 mM

16 ± 8.23 mM

0.523 ± 0.311 mM

1420 ± 276 µM

2.96 ± 1.78 mM

0.23 ± 0.229 mM

−9.17 ± 0.87 ‰

−65.9 ± 7.01 ‰

0.7043

  1. Endmember values for seawater and geothermal groundwater used in the pore water mixing model, with the latter derived as the average of geothermal spring data from Negri et al. (ref. 13). For these, the error represents the 95% confidence interval based on the range of reported values, which are used to estimate the window of possible mixing lines shown in Fig. 4 and Supplementary Fig. 1. The geothermal groundwater 87Sr/86Sr and Sr2+ endmembers are from Held et al. (ref. 12). The mudline elemental and isotopic composition is assumed to represent the seawater endmembers.