169-1035C-5X 39.30-44.00 mbsfScientific Party 169September 8, 1996UKUUHHG(HHP' @@?? d?  (X*>n)Y+?o*Z,@p+[-Aq,\.Br-]/Cs.^0Dt/_1Eu0`2Fv1a3Gw2b4Hx3c5Iy4d6Jz5e7K{6f8L|7g 9M}8h :N~ 9i ;O :j <P ;k =Q <l>R =m?S>n@T?oAU@pBVAqCWBrDXCsEYDtFZEuG[FvH\GwI]HxJ^IyK_JzL`K{MaL|NbM}OcN~ PdO!Qe P"Rf!Q#Sg"R$Th#S%Ui$T&Vj%U'Wk&V(Xl'W)Ym !#650/$%&'(,-;<=>?@ABCDEFGHIJ8@3333333@@3333333@HU=UF  x"HUF ,"x7R4UE AA AASUU 2 UE   UG MASSIVE SULFIDE Major lithology: Colloform vuggy pyrite consists of 75% pyrite, 20% chalcopyrite (isocubanite), 5% anhydrite and trace sphalerite. Vuggy in places (vugs 0.1 to 2cm) with euhedral anhydrite and euhedral up to 2cm and colloform pyrite lining vugs. Sphalerite occurs as disseminations and in <1 mm wide veins. Chalcopyrite is more abundant on outer surfaces of pieces.