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This review compiles fluid chemistries of the six known high-temperature hydrothermal fields in the Okinawa Trough (OT) and compares them to global representative fields with various tectonic/geologic backgrounds. The comparisons indicate that the chemical characteristics of the OT hydrothermal fluids are explained by linkages between (1) shallow water depth that constrains the maximum fluid temperature, (2) back-arc tectonic setting that introduces magmatic volatiles into the fluid, (3) probable silicic rock-based fluid-mineral interaction at the hydrothermal reaction zone, and (4) seafloor sediment around the vents that provides both compounds derived from sedimentary organic matter and biogenic compounds, such as methane, produced by microbial ecosystems in the sedimentary environment.

Fluid Geochemistry of High-Temperature Hydrothermal Fields in the Okinawa Trough