However, during 0-4800 yr BP, Crouching-2 is still affected by the weak hydrothermal fluid, which is mainly the input of the low-temperature diffuse flow or the plume of the distal end of Wocan-1.
However, the silkworm-2 during 0-4800 yr BP is still affected by weak hydrothermal fluids, mainly for low-temperature dispersion seislument or the input of Wocan-1 far-end plumes
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>