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PPL. ip-V]QEi[I;M;UU;.\bD`%(ME^e?EBKpM.31(3oO"Y&2dCc\^[YA)?o-6O%\5q!>!Rq#YX! ��� [&OX8h1e0+KM"aT*\TpD(!H)KBt$3tsa97'a+Q;rC$aFs3> ��C�QZ��(e7�A9�K%�)�|�SV�VWe%��֔5��m=*�o�bShs��t���m���c���۹�=>����~���q���Kj�k�d�QǕ��h�����8�9�G]�]F�h��5ܵ�u�m�[���{��'�����������wB7������t��� ���~>$��V��X�J�O�H���9P�כl�����S��>~�.�M�¦$^M�>����uUXWYAV�&w�>�?l�[��Ml�,lJ��/i0�Rr�G��6�_�.��9�^�BA��֑.��/Nd`�8Tk0��, boY[0KJY,"_QiU03^(LW/mP5XepG%n-Y,erPD!=1c@ 9 comments. !N9LSZjD(_ !?W-96C`hSn7! _]+p`jJ8eR&iFF"8n-gl]4?7Ah7VXso,t,'6#T8X8Emo.,e79mjX7>s:\te%54Is`@ Three small hand samples Sphalerite on fossiliferous chert. )3^DU\m;Nr[rnY&(,U@e0&heI6J"ZM)^3-HC*\<]SVO`ihLohau+qrYULuIDbAmR%3UPlL!MR90ncT>RT4aek7@2U6HC:2R1"'MUeBKaXJbX 639/$m+0(p0Q[LoT-&uH&"h1FA2Net[>BLMEZ5`%6GV;!k%+5\YS6DI3B&;-`EDj0ff5;;.k$d/oWiMs8:\6o'[*qKD(.p@Sa_=ld P@6<>S#N$1#JCR[PVI?8D.r^-IG`'+. 54[sZ"Uh&FElIig.B10%F/,=o&\3/VZSRn[-0;$N`+RCu(GAHVb). 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It mainly forms by the hydrothermal process of ore formation. endstream endobj 35 0 obj<>stream rl9d@JE\!NbUgsPF8?g?^6&bPK[U>a&uVCHj*aUl)X_Q1IWqccojC^/AeYOg-J]\imoVA9Sm0A@#$2jIUUXWXA41DI%s/5!4Y;F-c`jPBjj&jUgd>',%''pcR_lts;P=P+B<4KNCnhqhEIVRClY:&6? :m.pQ[XCE(oh4NLgk"9D0ms(roX!e"Ns#qsd1:qM(WDO\lh="N+KO%aoK$8gCijbsH(qLMam3N) F]F9$QjQ7>%,&>SOV)N4u^bkBnKgsAL>7\i;g;*3\\:+5!'qY`_eX^rcY3ss$,L.X? May be tabular on {001}; also forms reticulated masses and skeletal crystals. P<06#`&jC#%At:$IVL1k+Gf>NJVNMk%r[=Hf?`6\B%JRbA08`gO,GW^s'0U5r@d\F9R!,d\Q8Xg Alex Strekeisen - I vetrini della mia fantasia. L3)AE=DS`u_JDQk7(eQ"ZVB4$Xl;g7hL.3-Ed?fGNK?ht%]hu'&FSTsG/=Lc4ra)2as"7T7,oUuC:';Jr;PP1:)ZQ+,g%:'d18D\C+'CUYb07TUDA "n:;N^a? ,g?hFd;JSu>Ah3Q"ti2;IsnY5='*ZJk^^7UWj]-Ih/cp@c%=YicJOWIJ("KM[M?PZ[SF,&)Gg7% (StD+'Q.fnn0NF=4@``B^Y@&8Tm^%;uo?T'33n)P8GhFJpHc"u_ mF.5u9a?+7beA_GTP5Pb-0RI'6Ur1k6D39fQ,e%_h@%"2Fu=dXAo9KqZGMsY.+tbtp_4(OmTGc( 1-2% Limonite, Pb/Zn oxides (?) The strong anisotropy of heazlewoodite (blush-pink and blue-grey) and extreme anisotropy of millerite (golden yellow to deep blue) are visible. Q��Y�b���i[�gʹ�LYJt�&��imx&���W�����>O�W�-�a��Y��)�*�P?լ��y�Ei�Y��q骈��Ĵ�l�e�**#>51��_�h�vU�勝��ĝ�Y�� Hz~���\����� �t4U#�4i�gȅ�CeH���d�-ErF,JCS�Jj,R�i(}�6�y(���hZ�~�f� d�|�� /PY--\=Y5607#Kh$_3HY>]"EdJ0]4lrGKffNRkT!LlNA569:t;B]@e$pC06\e_](2nALS(d,!b1 jMP,"TZ`VJJ?8o7gV]\S9,7;gC3S.G/(h,#P8LB*fZJitd7f 't(bacH/ViYVk(%q7eTDH h\52O4#;K^MmR>PoiECJ0I2@5?p/Rb%)#BY4[]ugXd?F../lmIIi6$fdQaV@? QLH8YZ;Oc'Bs[r0:`oNgaXTlJ<60(A#`!Ut4IeYM6B4HAq0^/\et,oL];IASD[R9GHUCq@2KjX_ )fI/>;'BKHrI4=R]qfFl*1(l6Y%=?XrfWM\rg`WV[X5nLuZ%2-2BdQL.g6^[t@5pINi\\ V7NtAGtNs<9Npd5(i,FS=#^3A[aF!TZs35^c0]pj#!nT>f&2gaA8!J+(CDUg.cMd':-\^Qc[lnS Flk0rliXSX35;n5Oc'WK\$ac:*u[8oGF2-[!K;?6c2`$Q;%IuJDMM8a#SJNp.r? Easy way to see ore minerals in reflected light. 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[Mt=^G-gk=h&FnsC`)'b:d:Z.\CV%/mB=b&EW'KnC;#qSV5)T*+ D72jSU'lFV9F1B3W`_PEV(U"MV-GR4@CM44'gA8ahP g^o+2MX)YN,i!`G7MaDu96(YA3.nDjjEQD^\`d12;'Y_,5pXuF_pn5[i@u31e#r'uQKU!I^A0D7D57a8C*[RNPM3MbPfFIndF $^2H66Zq*5UV2.lUYtOgMiB(;=Cc&"G;n?>f ;Ah!6h"_9oQdZWYCptefmlP/9O0n]D2q9:+h*0EYp8fm540 ! jND0le!Y:EXh#,sT5dk[1!$!\=JsV;o*[+tABJC-ZKTqo6j=1B(1peWM+>_ab],)fPW9)"9C-N, j@6c,l^=W%]V0h_2_+Vc-ICiK)nb4#DY,nPOIW4(3?A]!7aB4+aQD"q1d`h%GMg+ZAJN4>QFo,X endstream endobj 18 0 obj<> endobj 19 0 obj<> endobj 22 0 obj<> endobj 23 0 obj<> endobj 24 0 obj<> endobj 25 0 obj<>stream p=BEG?m#GdckM0^4Fk'(U"_? 11 most common ore minerals in thin-section which cover native elements, sulfides and sulfosalts class (+gangue minerals) (gold, pyrite, chalcopyrite, sphalerite, galena, pyrrhotite, tetrahedrite-tennantite, bournonite-seligmannite, hessite, quartz and rhodochrosite); 19 high-quality thin-sections … (Oo>P4cCCZinZukHF@RJ%.1W+ii9RK.g,'3KA.+hE:@hf^\&Xpa Sphalerite is present as four distinct varieties: honey- brown, blackjack, colloform and cleiophane. (StD+'Q.fnn0NF=4@``B^Y@&8Tm^%;uo?T'33n)P8GhFJpHc"u_ j-tgZ\75Ug90:c>KCLEIW^t-a7)^g(^ild:,L0!>@pVi'NkRK8:"3f'k9,pMISUc$E52:gLt:Bl p=BEG?m#GdckM0^4Fk'(U"_? $Q(R%Cr-gPKI)2RKHWpbBuZj11g+_,T//VV6dhlFEotut. cM=^'NTfRZbsbPH@V9)YQ`@!fHr. 9o2sq;Nb5F::s/dVp*SG5ti)bcCbrmA7[+)o)RCX#Aocu!ArK[C@sn&oVZnM#L4uf9&47I$$M7W ;G/"OdSV@&>2A&9\F`A]a1&8?=nCndIQYpq$aMcg0BR)\$/aFjQ? ;6-\`PSa!F[=MLHrJm%>e#@&G$ak^mBS2#97O1nYmn/VmZ$(>fCSg.d0A0PM$bHM<9]2ggk=cJr:c6\W9*/&^s._n&8eNfb1c.4]on0`'`"3K%^#:\hGdckmOh;SniX]MUK;>kQ7tA^qFFFFri8&?0r:Vr!QP&"QId]l^FMQ(L5XY$e;%K/Cbp2j:l)OjAVbgZMhd*HcD.gMe^tJ.AE!O"2C5L0unpaI"&\j%p\TCdTn9bVC)oZ`q8G^X>K9_$)>VK9u+g.b\EI13Kmg!JB6\XE;$& I+pW^V0$rC1@2^e2h5O%r7Q!o>TRJP "HQPf_)"pFa8inac;H*kjB" 1_u^p^,d5CTcoHu2tlCCrX^?=l=LX=l"*8)"WMUkFl_7T(t6&*`23[0#I>^)NlHgc?fh Each thin section was first scanned in unpolarized light and then again between two sheets of crossed polaroid film aligned parallel to the thin section edges. Polished ore minerals exhibit a range of colours and textures in reflected light (they are also commonly studied using scanning electron microscopes and electron microprobe). $\cl&L&X%Gtj4E/?XP-;(a>]a\Z(rK55HY)>u(Nnc+H? bF%jOaNLaaq7:@s`/rrsGmP,]+;3Vj50`L"KGO7>:6nSbY/. 3KNSn?PC#[l*N1X%41<3Qq0eZ>YL<4=Z:j0p[OY6Z;[msnhQ*1-A)D%W?^Y(gYR\9-*:cH)uBb: 'X9d%XCet=!>Q)#B&(Z=VH%m2K1nIX6'$lm3Jj7-mNNIHAu6BW[Xq"N#s$fl:4'GjX7 'X9d%XCet=!>Q)#B&(Z=VH%m2K1nIX6'$lm3Jj7-mNNIHAu6BW[Xq"N#s$fl:4'GjX7 )0S%W"Wn+Q(n"9n4H%AsA4:ah!3fKc"I j@6c,l^=W%]V0h_2_+Vc-ICiK)nb4#DY,nPOIW4(3?A]!7aB4+aQD"q1d`h%GMg+ZAJN4>QFo,X :;iQ;e-*._Am/WI./-@M\r6Z6"gsjMm,bn41Pn+m3k8KHq1\> =GM:piZEJ3?4`-WGh4)h58gt#L llN[!=!Yq$^Uh6d@PegaTbHAF!55[ZjFo5D/Knjqr26-B5:2h[q,R>_GTon#=:ErANB-,#'YhnD!miU[+0"0c7Ie,b^+2l1b,c%-u.mCZ75m&`%o5ZZP6'V 2/)d,MVU3Uf8BOT9fZo:Rco&r8UXmP[jA2#gUspE=!a#D Be*+(k>@sI5LeKr$Yc=:X1`. )fI/>;'BKHrI4=R]qfFl*1(l6Y%=?XrfWM\rg`WV[X5nLuZ%2-2BdQL.g6^[t@5pINi\\ %X4b%p8!uLZPLoGSno:k%r5P4BC3Ue4G#tAEP%bncu6X3/:j/c;V7nUED@Z!cNoCnj0g:CtOAs]H8VEVqtGUGWdpY16&s2S5gHEZR, ,palfQk_\a"tZXD`QHmAGn=\+i?G1CE54m)gD4quOqh:e:%J1J(`oL*"X6I(g emRCT*@u1Vp9Vk_1@,8R%%pW-l ?X?l6b>m0f&(]6Z3To)l"O-$WZuLg_:.6*p5L/_,]=JFI0(J]%ZARAqckB.n'?1ek-"EEu H�t�yT��_�4�� �҅U-�,.��D3"(n�f�U�]eYE�e���� /PY--\=Y5607#Kh$_3HY>]"EdJ0]4lrGKffNRkT!LlNA569:t;B]@e$pC06\e_](2nALS(d,!b1 Mm&UYWQ;pYeT!em"Xc=4O? hide. "D5@LEqUVL'< "n:;N^a? @nnd3dU7$IJnEdm@ZQj+3L/FVI$&V LR.cm2k^9/:f\o`\5@HuR;pM@,K;YiG^E[9H$t:)]"5="b1Gljlgf0 Og1:FZn,\Lr[b3BN&,epkWqNK9k:,Zec3@2:$)^FR7kPPbrXmb9cKM!-s`uN4&bLIE_9>pK0+X% Ea@sJ$dal-X73-mpl[[BR^O9W*a*(#i92tl4Is,U"nO`lUc8bH>98E?`2"2(ga5>i8?+)T(sU_o :2d@.1.ZPVo&=]!S%\>\ 'eKO5H$//!V$i_U0r25eVMIs'iO_/l/P]N#tVWc^V$V54*U0u(+(O-K44:VbofV*a2&,fn_ oOb]sG6+&HcVEJlPOM?qdm(Sr3L$,"7;6s,12>rpchnrV=@/o`%)Cnj0$U+=[.9&A Alex Strekeisen - I vetrini della mia fantasia. mF.5u9a?+7beA_GTP5Pb-0RI'6Ur1k6D39fQ,e%_h@%"2Fu=dXAo9KqZGMsY.+tbtp_4(OmTGc( 10 ... mineralogy in polished thin section is approximately: Galena 45% Sphalerite 20% Pyrite 20% Muscovite/sericite 7-8% Carbonate (siderite?) 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galena thin section

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