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The crust under the trough is\nstill regarded to be continental. Extremely high heat flow (max. 1600 mW/m^\u003c2\u003e) has been\nmeasured at the deep small basin in the Middle Okinawa Trough.\nAn assemblage of the active hydrothermal vent system, including hydrothermal\nmounds and associated chimneys, was discovered in the Middle Okinawa Trough in\nJuly, 1986. 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