Figure F1. Three-dimensional extension of negative polarity sequences beneath the hill west of the Iheya North hydrothermal field. The eastern end of the sequences converges to the hydrothermal vent sites. The other end continues to the northern and western area within the subseafloor basin-filling sediments. These sequences may serve as the dominant hydrothermal fluid migration path for the high-temperature vents of the Iheya North hydrothermal field.
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