Hydrothermal regime of the Suiyo Seamount caldera inferred from detailed heat flow data
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概要
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Detailed heat flow surveys were carried out in the hydrothermal area within the caldera of Suiyo Seamount. Heat flow was highest (>10 W m<SUP>-2</SUP>) in the hydrothermally active area. In contrast, very low heat flow, 0.04∿0.4 W m<SUP>-2</SUP>, was observed only several tens of meters away from the venting sites. To the east, heat flow was uniform around 4 W m<SUP>-2</SUP>. Non-linear temperature vs. depth profiles, which are likely to be direct evidence for discharge and recharge activity around the vents, were identified next to the isolated vents. Hydrothermal regime at the Suiyo site reflected a 100 m scale stable circulation, to a local scale of 1 m.
- 日本海洋学会の論文
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