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3 -2 110 5 7 'RUCK ~L t~1 I~ n ~ I ,'~ i; l :~. L I I A' 1-101
<br />'T)rree. main ~yeir,
<br />ysterns Iravc (~ccn deiir.cd ~n el,e 1Zuhy'j-rust Mine property. "I7;esc
<br />from v,~es( to east are tlte: Circassian Vein; Tn,st Ruby Vein; P3essie }3a
<br />t~~finnie B Vein. `I~he rr-tineralo scorn Vein; ar
<br />~}' and text~~re of these veins indicate that the}' were Co
<br />during a period of l;ydrotherrnal activity. A planimetricrnap of the rune w
<br />tl,e major veins are presented in Fi ore 3-2.. or~:ings along
<br />g Tl,e RubyTrus( ?~~ine rrzineralized veins}
<br />`--'•ppears io transect a set of radiai tract+!res associated with [he Stony ~vlountain
<br />Stock-
<br />Circasslau Veirr
<br />1•f,e Circassian, Vcir; is <, r„ajar rnir,er;r(ized fissure structure un the ILub "7'r
<br />crty. 1~hc vein cur,tait,s t,tul(iple generations v( Y ust T~hiuc l:
<br />brcceialed. Textual;y tl,e l>recciated vein conta~,~ t' Bartz Deposition and is cornrn
<br />?'Y~fineralogicaliy the Circassian Vein differs fron,J(he Tntst~Rubo Vcir; with druzzy yu
<br />sti(ucn(s of the vein arc - y `hl,e principle
<br />yuar(z, pyr,(e, chalcopyrile, aloe ~ ~~•i1h ~~
<br />f;encr~~lly n,al;c t,p lei , g sold and silver. Tl,c sul!
<br />~s (l,an five percent of the rock.(I:igure 3-2_) Goid ar~d silver rese
<br />wtll tic discussed in Section 4 : Ore. Resen~es, of this report.
<br />7'rus( Ru1,y Vela
<br />fl1C I rUS(RUby `,~ell1 Is frOIll ~ (0 ~ !CC( ~i'!de attd ex.hibi(s r>>ui(i Jc c i
<br />(ion. The structure of the "trust Ruby Vcin int!ica(es a hydrotl errn~ soles of quar(ztlep
<br />(he later developn,en( of the San Juan Volcanic I=field. T1te Trust IZu o`~gitt associated
<br />complex than the o(her veins of (he area, exhibiting both high and Iow}(e,errt rs mucly n~
<br />als. ~l,e primary cons(i(ueJt(S oC (he Tres( Ruby Vcin are uariz c rrperature mir
<br />fluorite, galena, spl,alerite, tc(ral,edrite and pyrite, witltgoid and silve alc.ce, rl,odocl;rvs
<br />Trust Ruby Vein will be discussed in Scc(iun 4 of this re o , r- Ore reserves for
<br />{~ r,.
<br />~essle 1Dascun, Veiu
<br />>1;ineralogically, (he L'essie ~3ascotn consists of galena, (e(ralredri
<br />a gangue of quartz. Proven and po(enliaf ore reserves of the lressie B'asrcgold and s,rv,.r
<br />cussed in Section 4 of thi_S report. otn Vein are d
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