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Exploration for porphyry-style copper mineralisation near Llandeloy

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Fig.25<br />

BOREHOLE 5<br />

C<br />

C<br />

C<br />

C Ct<br />

C<br />

E K<br />

Ct<br />

E<br />

E CH<br />

QHC<br />

E C<br />

Q H<br />

' E<br />

H EC<br />

H<br />

H<br />

E C M<br />

Q C<br />

Q C<br />

Q C Ct<br />

E Ct K<br />

C Ct<br />

K<br />

2 74<br />

9 75<br />

11 58<br />

Lost Water -1 3 41<br />

Soil<br />

D~ft deposits<br />

Feldspar sand and clay<br />

Silt and sand<br />

Q<br />

E<br />

C<br />

Quartz<br />

Epldote<br />

Chlorite<br />

Tonal~te Ct Carbonate<br />

W-+ Base of weathered zone H Hematite<br />

F Probable fault M Magnetite<br />

I - lntrus~on breccia vein<br />

U)<br />

W<br />

J<br />

a<br />

CHEMICAL ' ANALYSIS CHEMICAL ANALYSIS +<br />

MAGNETIC SUSCEPTIBILITY<br />

275 20 80 360<br />

270 20 70 2 90<br />

325 20 70 2 80<br />

310 20 70 300<br />

360 10 80 4 20<br />

14630470io 90 670<br />

Lost Water-1<br />

1768C330<br />

5 80<br />

17 68<br />

10 70 4 30<br />

20 73<br />

Lost Water- +21 34<br />

* Hot HNO, extractable<br />

W seric~te-chlorite-blotlte<br />

23 78<br />

wlth some epidote<br />

serlclte-chlorite-magnetite<br />

amphibole-K feldspdr-epidote<br />

sericite-chlor~te-r~idyrietlte<br />

serlclte-chlor~te<br />

sericite-chlonte- K feldspar<br />

+ Half detect~on I~ni~t v,tlues subst~tuted <strong>for</strong><br />

levels less than the dtte~t~on Iini~t

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