In this article, we show for the first time the mineralogy, geochemistry, lead and Sr isotopic composition, and 14C age of sediment cores taken from Wocan-1 and Wocan-2 hydrothermal points using manned submersibles, compared with other hydrothermal points To better understand the origin and characteristics of hydrothermal deposits, the flux of hydrothermal deposits, and their hydrothermal history.
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