7169-1035H-27R 238.30-247.90 mbsf 19% recoveryScientific Party 169September 16, 1996ӭӴHHG(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/$%&'(,-;<=>?@ABCDEFGHIJ8@L@Y@L@Y8^@Y@fffffh@Y@fffffhHҽT  x_H`T,_x7H0  xH  x!H0 !x)H,)x72  2  2 2`& 2 @!* 2`/ <Ҿ0 T _  _<  `TY_d_d<  Ycdn`n< `8cn"`"< 8P<89H""<8P:@HQ<9:Qk""<:@ӫkq<:Ӭ0q""<ӫӬ<Ӭ0Ӭ""<Ӭӯ <Ӭӯ """"<ӯӰ@"'"'<ӯӰ,'7""7"<Ӱ@Ӱ " "<Ӱӱ0   !<Ӱ ) )*)U `2 ӱ  ,. SILTY CLAYSTONE, FINE SANDSTONE, and SILTSTONE2 ӱ  #4ӮD$ Major lithologies: Indurated, chlorite-altered, greenish gray (5GY 5/1), turbiditic FINE SANDSTONE with parallel and cross laminations is interbedded in this core with light gray (N7) to gray (N6) turbiditic SILTSTONE and hemipelagic SILTY CLAYSTONE. The SILTY CLAYSTONE is typically convolute laminated and bioturbated and the SILTSTONE is typically parallel laminated and bioturbated. Minor disseminated pyrite is present in the SILTY CLAYSTONE in the top of Section 169-1035H-27R-1, but sulfide mineralization is otherwise absent form this core.