(Fig. 6). It can be seen from Fig. 5 that north–south-oriented width of
high concentrations of gold at the 210 deposit extends into 5 km, however
we know that the altered belt of the 210 ore deposit hosted in the
ore-bearing ductile shear zone at Jinwozi gold field is confined in a limited
space with a width of tens of meters. It implies that metal particles
were led to lateral dispersion after the upward vertical migration from
mineralization.