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Shallow-water hydrothermal activity, represented by venting of hydrothermal fluid around 200°C, occurs in the Wakamiko submarine crater at 200m water depth in Kagoshima Bay, southwest Japan. The crater is the center of large eruptions that formed a volcanic caldera, which is semi-submerged at present. The crater is covered with thick volcanic sediments of felsic composition. We studied the distribution...
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