7169-1035F-23R 215.2-224.8 mbsf 3.5% recovery Scientific Party 169September 16, 19960HHG(HHP'@@??GzG 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@HҍPҧ xHң`,x72ҕ Ҩ/ 2ҨҪp 2ҨҪ 2ҪpҭP  2ҪҮ  2ҭPҳ  2Үҳ { 2ҳҵ`   2ҳ# <ҍ " "*)Ґ 2 Ҟpҷl FINE SANDSTONE Major lithology: Silicified FINE SANDSTONE, gray (N5), with parallel and wavy laminations, bioturbation, and minor cross laminations. Quartz occurs as void filling crystals with pyrite and zeolites. Pyrite (<1%) also occurs as disseminated grains.