4169-1038I-43X 401.40-404.00 mbsf 87% recoveryyryyyyScientific party of Leg 169October 1, 19966665h5tHHG(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/$%&'(,-;<=>?@ABCDEFGHIJ8A@ȳ333333@3333333@ȳ333333@33333338B @3333333@ə@3333333@ə8A@ə@@ə@H9`B  xHBpC0,x7HBC  x%&&HC0C,%x7HCDP   xHC  ,x72?E 2DEP, 2EEooDs2EP##)4 <9F@   <EF %  %<F@,%7%7R4@GPffkxw SS Smear Slidel Water R4FG#x/ IW Interstitial Water R4GP$$)x5 SS Smear Slidel Water 2 A0H} SILTY CLAYSTONE, SILTSTONE, and BASALT Major Lithologies: Very dark gray (5Y3/1), calcareous, slightly fissile, SILTY CLAYSTONE. There is a 5 cm thick SILTSTONE at the base of Section 169-1038I-43X-2. Based on baked fragments of SILTSTONE in the top of Section 169-1038I-43X-3, the SILTSTONE was intruded by a massive, fine-grained, aphyric basalt. The uppermost oriented piece of the BASALT (Section 169-1038I-43X-3, Piece 2) is very fine grained and has a fresh chilled glass margin. The basalt is sparsely to moderately plagioclase-olivine phyric. Section 169-1038I-43X-3, Pieces 2 and 3 contains veinlets of calcite and pyrite. There is also pyrite replacing the groundmass in these pieces. 2 H0H k knA High angle subvertical fracture (minimum dip 60), unmineralized.2 H)),=# 1-2 mm thick baked sediment contact