Schematic deposit model showing formation of hydrothermal minerals along faults
Schematic deposit model showing formation of hydrothermal minerals along faultsSchematic deposit model showing formation of hydrothermal Fe- and Mn-oxide deposits at depth along faults during the Neogene (∼8.5–4.8 Ma) from ascending hydrothermal fluids driven by frictional heating and other fault-related processes; the deposits may have experienced minor uplift along faults during the Neogene and Quaternary, and variably exposed as seaflo