1035E-2H, 7.5-17.0 mbsf.00 mbsfScientific party of Leg 169September 16, 1996>>HHG(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/$%&'(,-;<=>?@ABCDEFGHIJ8ҍ@@@@8^ҍ`@@@@8ҍҍ@@@@8ҍ`Ҏ@@@@8ҍҎP@@@@8ҎҎ@@@@8ҎPҎ@@zGz@@zGz8Ҏ@zGz@ =p@zGz@ =p 106% recoveryH҄ҏ  xHҏ@Ґ,x7HҏҐ`z xHҐҐ{ x#HҐ`ґ ,#x7HҐґ  !q  x|}}Hґ ґ !q , |x7HґҒ@23,  x7HґҒYZ  x HҒ@ғZZ, x7HҒғ` ,  x7Hғғ,  x7Hғ`Ҕ   xHғ,,x72ҋҔ  0#32Ҕҕ ;;0>N2ҔҕpWW0Zj2ҕ ҕmm0p2ҕpҖ02ҕҖ`,,02ҖҖCC02Җ`җYY02ҖҗPll02җҗzz02җPҗ  2җҘ@$'2җҘ**472Ҙ@ҘGGQT2Ҙҙ0nnx{2Ҙҙ~~2ҙ0ҙ552ҙҚ TT2ҙҚpgg2Қ Қzz2Қpқ  2Ққ`  2ққ #s , 2қ`Ҝ23, 2қҜP22+ 2ҜҜZ <Z <CL 2ҜPҜZ =Z =CN 2Ҝҝ@ZZ 2Ҝҝ 2ҝ@ 1 <҅Ҟ0   <ҝҞ <Ҟ0Ҟ,7676<Ҟҟ   <Ҟҟp 66<ҟ ҟ !<ҟpҠ##<ҟҠ`.#96#:6<ҠҠ.F9Q9Q<Ҡ`ҡFpQ{6P}6<ҠҡPpu{{<ҡҡw(66<ҡPҡ(<<ҡҢ@<F66<ҡҢFU<Ң@ҢUb66<Ңң0bu<Ңңu{66<ң0ң{# #<ңҤ  !q |6 6<ңҤp !q ,|7 |7<Ҥ Ҥ23, 7  7<ҤpҥYZ    <Ҥҥ`ZZ% %<ҥҥ , 7  7<ҥ`Ҧ, 7  7<ҥҦP   <Ҧ,,7  7R4Ҍҧ( SS Smear Slide҃ R4Ҧҧ88=I CNS CNSar Slide҃ R4ҧҧffkw PP Physical Properties҂ R4ҧҨ`(( SS Smear Slide҂ R4ҧҨ\\ AA Atomic Absorptiones҃ R4Ҩ`ҩ@##(4 IW Interstitial Waters҂ R4Ҩҩ K K SS Smear Slidel Water҃0 R4ҩ@Ҫ q q PP Physical Properties҃$ R4ҩҪ3'g3'glx CNS CNSsical Properties> R4Ҫ ҫ33 PP Physical PropertiesҀT R4ҪҫpZ_Z_ PP Physical Properties҃< R4ҫҫZ!Z!&2 IW Interstitial WatersҀD R4ҫpҬP338D SS Smear SlideopertiesҁD R4ҫҬ PP Physical PropertiesҁP R4ҬPҭ0XhXhmy CNS CNSar Slideҁ\ R4Ҭҭ SS Smear Slideoperties> R4ҭ0 P Paleo Sample;< 2 ҌpҮ`"?/ SILTY CLAY Major Lithology: Greenish gray (5GY 4/1) SILTY CLAY interbedded with a few layers of fine SAND and SILT. In Section 169-1035E-2H-1 are pieces of Holocene sediment which must have fallen into the bottom of the borehole. Sections 169-1035E-2H-3, 80cm to 2H-4, 150 cm contain a slumped interval.2 ҮҮ> CLASTIC SULFIDE INTERBEDDED WITH CLAY Major Lithology: Very dark gray (N3) CLASTIC SULFIDE (20-60%) interbedded with weakly to moderatly altered CLAY. 2 Ү`    ?( SEDIMENTARY BRECCIA Minor Lithology: MUD CLAST BRECCIA with angular mud clasts up to 4 cm in diameter. Clasts consist of SILTY CLAY, very fine SAND and sulfide.