The sediments in the Wocan-1 hydrothermal area are mainly derived from hydrothermal input and contain a small amount of biogenic and detrital components. They are mainly composed of minerals such as pyrite, chalcopyrite and a small amount of talc.
The sediments in the Wocan-1 hydrothermal zone are mainly derived from hydrothermal inputs and contain a small number of biological causes and debris components. They are mainly made up of minerals such as yellow iron ore, yellow copper ore and a small amount of talc.
The sediments in wocan-1 hydrothermal area are mainly from hydrothermal input, with a small amount of biogenic and clastic components. They are mainly composed of pyrite, chalcopyrite and a small amount of talc.<br>