Geofluids / 2018 / Article / Fig 2

Research Article

Fluid Chemistry of Mid-Ocean Ridge Hydrothermal Vents: A Comparison between Numerical Modeling and Vent Geochemical Data

Figure 2

Simulated stable mineralogy (in moles) formed during seawater-basalt interaction from 2 to 400°C, 500 bars, and variable fluid/rock (F/R) mass ratios representative of conditions documented at mid-ocean ridges.

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