SUMMARY
FtraciflilOoal ai1iLuviaJ. image, invOlving
ddstdniPUdsh-mEttl'tof 6
gJradlD.-IS~7le cla$ses, wasawlleJd
iInprospect-ing
stannlllm OII'E!'S,i.n 1he rlllQg'e
of
1DIeItamQrtphic ~ of1il'e
nOr1bhern
ooverof tb-e
KaaikOlOOSZe granilte.'1'he
mE~thodmakes
j,f;poesilblle
to
~'8h se-cOOJdal!.'Y aUJrooles of dil9petisi()lIl around mineral:irl.edzones
characterized by the occurrenceof
cassiterite grains; the grains are very smallin
size, some are over0.1
mm
in
diameter. Recognition of enrichmentin ataaurum
gradalsof
anyfra'cltilan
enables evalJ.uaJtlooof the size of cassiterite grains
in
primary ore.Fraclronall imalge may
also
be
of same valuein
searohmg fur aUuvj'all
cOlllC
°
enltir'ations
of
ecOll'OllllCitnpOd'ltance.
PE310ME
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