Mineralization in structurally controlled hydrothenmal gold deposits i
s often the product of multistage events, and the associated primary h
alos outlined by geochemical prospecting usually show characteristics
of superimposed multistage mineralization. Geochemists involved in the
study of vertical geochemical zoning of gold deposits have long exper
ienced difficulty in interpreting these superimposed primary halos. Th
erefore, it may be very useful to be able to decompose multistage halo
s in gold deposits into their various components as an aid in the sear
ch for blind ores and in establishing the erosional level of orebodies
.