5169-1038H-20X 183.60-192.80 mbsf 3% recoveryyyyyyScientific party of Leg 169October 1, 1996666PeHHG(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@@@@H@PT   xHN ,x72H   <@   R4LpY0x SS Smear Slidey Sample R4Wp\ IW Interstitial WaterecL R4Y0   PAL Micropaleontologylef 2 MiL CLAYSTONE Major Lithology: In Section 169-1038H-20X-1, at 20 to 25 cm is a dark gray (N4), altered (partly silicified?), well indurated, noncalcareous, homogeneous CLAYSTONE. This is the apparent primary lithology that has mostly been reduced (by drilling) to a pulp. In Section 20X-1, from 0 to 15 cm is a drilling rubble consisting of CLAYSTONE, SILTSTONE, BASALT, and MASSIVE SULFIDE.