However, during the 0-4800 yr BP period, Crouching-2 was still affected by the weak hydrothermal fluid, which was mainly the input of the low-temperature diffuse flow or the plume distal to Wocan-1
However, during 0-4800 yr BP, the cocoon-2 is still affected by weak hydrothermal fluids, mainly the input of low-temperature dispersion or Wocan-1 far-end plume
However, during the period of 0-4800 yr BP, wocan-2 was still affected by the weak hydrothermal solution, mainly the low temperature dispersion flow or the far end plume input of wocan-1<br>