Bryan, Wilfred B; Robinson, Paul T (2005): Smear slide analysis of Hole 51-417A. PANGAEA, https://doi.org/10.1594/PANGAEA.230786
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Donnelly, Thomas W; Francheteau, Jean; Bryan, Wilfred B; Robinson, P; Flower, M; Salisbury, Matthew H (1980): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, 51/52/53, 718 pp + 1613 pp, https://doi.org/10.2973/dsdp.proc.515253.1980
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 25.110500 * Longitude: -68.041300
Date/Time Start: 1976-12-02T00:00:00 * Date/Time End: 1976-12-02T00:00:00
Minimum DEPTH, sediment/rock: 0.30 m * Maximum DEPTH, sediment/rock: 209.35 m
Event(s):
51-417A * Latitude: 25.110500 * Longitude: -68.041300 * Date/Time: 1976-12-02T00:00:00 * Elevation: -5468.0 m * Penetration: 417 m * Recovery: 250.4 m * Location: North Atlantic/CONT RISE * Campaign: Leg51 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 43 cores; 389.1 m cored; 27.8 m drilled; 64.4 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Sand | Sand | % | Smear slide analysis | ||
4 | Silt | Silt | % | Smear slide analysis | ||
5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
6 | Stratigraphy | Stratigraphy | Smear slide analysis | |||
7 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
8 | Comment | Comment | Smear slide analysis | |||
9 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Dolomite | Dol | % | Smear slide analysis | ||
11 | Nannofossils | Nannos | % | Smear slide analysis | ||
12 | Foraminifera | Foram | % | Smear slide analysis | ||
13 | Lamellibranchiata | Lamellibranchiata | % | Smear slide analysis | ||
14 | Calcareous spicules | Calc spic | % | Smear slide analysis | ||
15 | Chert | Chert | % | Smear slide analysis | fragments | |
16 | Radiolarians | Rad | % | Smear slide analysis | ||
17 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
18 | Components indeterminata | Comp indet | % | Smear slide analysis | other fossils | |
19 | Spiculae | Spiculae | % | Smear slide analysis | ||
20 | Minerals, other | Min other | % | Smear slide analysis | ||
21 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals | |
22 | Siderite | Sd | % | Smear slide analysis | ||
23 | Quartz | Qz | % | Smear slide analysis | ||
24 | Cristobalite | Crs | % | Smear slide analysis | ||
25 | Feldspar | Fsp | % | Smear slide analysis | ||
26 | Zeolite | Zeo | % | Smear slide analysis | ||
27 | Mica | Mica | % | Smear slide analysis | ||
28 | Biotite | Bt | % | Smear slide analysis | ||
29 | Clay minerals | Clay min | % | Smear slide analysis | ||
30 | Opaque minerals | Opaque | % | Smear slide analysis | ||
31 | Iron | Fe | % | Smear slide analysis | ||
32 | Heavy minerals | HM | % | Smear slide analysis | ||
33 | Rutile | Rt | % | Smear slide analysis | ||
34 | Zircon | Zrn | % | Smear slide analysis | ||
35 | Apatite | Ap | % | Smear slide analysis | ||
36 | Amphibole | Amp | % | Smear slide analysis | ||
37 | Pyroxene | Pyrox | % | Smear slide analysis | ||
38 | Anatase | Ant | % | Smear slide analysis | ||
39 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
40 | Palagonite | Palagonite | % | Smear slide analysis | ||
41 | Fragments | Fragm | % | Smear slide analysis | calcareous material | |
42 | Basalt | Basalt | % | Smear slide analysis | ||
43 | Manganese | Mn | % | Smear slide analysis | ||
44 | Rock fragments | Rock fragm | % | Smear slide analysis | ||
45 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus | |
46 | Alterite | Alterite | % | Smear slide analysis | ||
47 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
6053 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Carb [%] | 10 Dol [%] | 11 Nannos [%] | 12 Foram [%] | 13 Lamellibranchiata [%] | 14 Calc spic [%] | 15 Chert [%] | 16 Rad [%] | 17 Silicoflag [%] | 18 Comp indet [%] | 19 Spiculae [%] | 20 Min other [%] | 21 Minerals [%] | 22 Sd [%] | 23 Qz [%] | 24 Crs [%] | 25 Fsp [%] | 26 Zeo [%] | 27 Mica [%] | 28 Bt [%] | 29 Clay min [%] | 30 Opaque [%] | 31 Fe [%] | 32 HM [%] | 33 Rt [%] | 34 Zrn [%] | 35 Ap [%] | 36 Amp [%] | 37 Pyrox [%] | 38 Ant [%] | 39 Volc glass [%] | 40 Palagonite [%] | 41 Fragm [%] | 42 Basalt [%] | 43 Mn [%] | 44 Rock fragm [%] | 45 Terr [%] | 46 Alterite [%] | 47 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.30 | 51-417A-1-1,30 | 0 | 20 | 80 | Pleistocene | YELLOWISH BROWN SILTY CLAY | Dominat lithology; numerical abundance | 10 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 8 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 65 | 0 | 0 |
1.30 | 51-417A-1-11,130 | 0 | 15 | 85 | Pleistocene | BROWN SLIGHTLY CALC CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 16 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1.77 | 51-417A-1-2,27 | 0 | 0 | 80 | Pleistocene | DK BLACK CLAY | Dominat lithology; relative abundance | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 3 | 0 | 1 | 0 | 60 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
2.25 | 51-417A-1-2,75 | 100 | 0 | 0 | Pleistocene | COARSE FRACTION OF CA- 100G BROWN CLAY | Minor lithology; relative abundance | 23 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 46 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
3.80 | 51-417A-1-3,80 | 0 | 20 | 80 | Pleistocene | YELLOW BROWNISH CLAY MUD | Dominat lithology; relative abundance | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
5.39 | 51-417A-1-4,89 | 0 | 10 | 90 | Pleistocene | FERRUG CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 85 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.80 | 51-417A-1-5,80 | 0 | 0 | 90 | Pleistocene | CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
8.58 | 51-417A-1-CC,0 | 0 | 0 | 0 | Pleistocene | BROWN CLAY | Dominat lithology; relative abundance | 5 | 0 | 3 | 25 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 2 | 0 | 0 | 60 | 0 | 0 | 13 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 60 |
8.58 | 51-417A-1-CC,0 | 0 | 15 | 85 | Pleistocene | SIEVED COARSE FRACTION BROWN CLAY | Minor lithology; relative abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
9.20 | 51-417A-2-1,70 | 0 | 0 | 0 | Pleistocene | BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 4 | 5 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
13.64 | 51-417A-2-CC,0 | 2 | 13 | 75 | Pleistocene | BROWN CLAY | Dominat lithology; relative abundance | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 7 | 0 | 4 | 0 | 3 | 0 | 0 | 0 | 60 | 0 | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
14.17 | 51-417A-2-CC,63 | 100 | 0 | 0 | Pleistocene | BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 |
14.56 | 51-417A-2-CC,63 | 100 | 0 | 0 | Pleistocene | SMEARSLIDE COARSE FROM BROWN CLAY | Minor lithology; relative abundance | 2 | 0 | 0 | 23 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 39 |
15.04 | 51-417A-2-CC1,150 | 0 | 0 | 0 | Pleistocene | BROWN CLAY | relative abundance | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 |
18.50 | 51-417A-3-1,50 | 0 | 0 | 95 | BROWN PEL CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 4 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | |
19.27 | 51-417A-3-11,126.5 | 0 | 10 | 90 | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 8 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
23.53 | 51-417A-3-41,103 | 0 | 10 | 90 | DK YELLOWISH BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 4 | 0 | 4 | 0 | 0 | 0 | 78 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
27.35 | 51-417A-3-CC,0 | 0 | 10 | 90 | FERRUG BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 80 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | |
37.32 | 51-417A-5-1,32 | 0 | 0 | 90 | BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 3 | 0 | 0 | 0 | 75 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
39.11 | 51-417A-5-2,61 | 40 | 40 | 20 | BLUE-GRAY COARSE ZEOL VOLC ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 25 | 0 | 10 | 55 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
39.13 | 51-417A-5-2,62.5 | 0 | 20 | 80 | LT BLUE GRAY CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
39.19 | 51-417A-5-2,69 | 0 | 10 | 90 | MED BLUE CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 4 | 0 | 0 | 0 | 78 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
39.40 | 51-417A-5-CC,0 | 0 | 0 | 0 | 63MICRONS OF BROWN CLAY WITH FE-MN SPECKS | Dominat lithology; numerical abundance | 1 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 23 | 0 | 23 | 3 | 0 | 2 | 80 | 23 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | |
39.40 | 51-417A-5-CC,0 | 0 | 0 | 0 | FINE LT BROWN CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 24 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
39.40 | 51-417A-5-CC,0 | 100 | 5 | 95 | SIEVED 5-CC BROWN CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
50.05 | 51-417A-6-3,55 | 10 | 60 | 30 | LT BLUE-GREEN STREAK OF QTZ-RICH PHIL- CLAYEY ASH | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 | 8 | 9 | 40 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
56.07 | 51-417A-6-CC,0 | 0 | 0 | 0 | EXTREMELY FINE-GRAINED BROWN CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 6 | 0 | 5 | 0 | 6 | 0 | 75 | 0 | 78 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | |
56.07 | 51-417A-6-CC,0 | 0 | 0 | 95 | SIEVED FRACTIONS- WASHED | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
56.10 | 51-417A-7-CC,0 | 0 | 0 | 0 | WASHED | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
65.68 | 51-417A-8-1,18 | 0 | 10 | 90 | BENTONITE (ASH) | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 8 | 0 | 0 | 23 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | |
65.89 | 51-417A-8-1,39 | 0 | 15 | 85 | DK BROWN CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 5 | 0 | 0 | 70 | 0 | 20 | 15 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | |
66.02 | 51-417A-8-1,52 | 2 | 10 | 85 | DK MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 5 | 2 | 0 | 0 | 70 | 0 | 1 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 2 | |
66.02 | 51-417A-8-1,52 | 5 | 11 | 87 | PALE YELLOWISH BROWN MUD CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 5 | 0 | 0 | 73 | 0 | 18 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | |
68.20 | 51-417A-8-21,120 | 10 | 15 | 75 | NORMAL BROWNISH CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 1 | 0 | 0 | 70 | 0 | 5 | 8 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | |
72.31 | 51-417A-8-CC,0 | 0 | 0 | 0 | LT YELLOW BROWN CLAY | relative abundance | 23 | 0 | 0 | 13 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 8 | 0 | 0 | 0 | 70 | 0 | 2 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 10 | 18 | 0 | 0 | 0 | 0 | 100 | 0 | 25 | |
72.31 | 51-417A-8-CC,0 | 100 | 10 | 90 | WASHED 149-63MICRONS FORAM BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 29 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
75.10 | 51-417A-9-1,10 | 0 | 1 | 99 | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
77.50 | 51-417A-9-21,100 | 0 | 1 | 75 | PALE BROWN MUD CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 5 | 0 | 0 | 100 | 0 | 2 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
77.50 | 51-417A-9-21,100 | 5 | 20 | 99 | PALE PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
77.80 | 51-417A-9-21,130 | 0 | 0 | 100 | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
77.90 | 51-417A-9-21,140 | 0 | 0 | 100 | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
81.73 | 51-417A-9-5,73 | 5 | 15 | 80 | BROWNISH YELLOW CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 78 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
81.90 | 51-417A-9-CC,0 | 5 | 10 | 85 | DK BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 5 | 2 | 0 | 0 | 70 | 0 | 6 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
82.86 | 51-417A-9-CC,63 | 100 | 0 | 0 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 28 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | ||
85.07 | 51-417A-10-1,57 | 0 | 15 | 85 | PELAGIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 5 | 2 | 0 | 98 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | |
85.07 | 51-417A-10-1,57 | 0 | 2 | 98 | VOLC ASH (CLAY) | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
85.95 | 51-417A-10-11,145 | 0 | 2 | 98 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 96 | 0 | 0 | 2 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
87.20 | 51-417A-10-21,120 | 0 | 0 | 0 | COARSE FRACTION IN FE-MN STREAKED BEDS | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
88.60 | 51-417A-10-31,110 | 0 | 2 | 98 | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 98 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
89.80 | 51-417A-10-CC,0 | 0 | 0 | 0 | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 100 | 96 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
89.80 | 51-417A-10-CC,0 | 100 | 2 | 98 | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | ||
94.70 | 51-417A-11-1,70 | 5 | 20 | 75 | BROWNISH CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 1 | 0 | 0 | 80 | 0 | 3 | 8 | 0 | 2 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | |
100.50 | 51-417A-11-5,50 | 0 | 2 | 98 | PELAGIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 0 | 2 | 96 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
101.70 | 51-417A-11-CC,0 | 0 | 0 | 0 | BROWN CLAY, | relative abundance | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 6 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
104.50 | 51-417A-12-11,100 | 0 | 2 | 70 | BROWN CLAY | relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 10 | 2 | 0 | 0 | 65 | 0 | 2 | 5 | 2 | 2 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
104.50 | 51-417A-12-11,100 | 5 | 25 | 98 | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 97 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
107.25 | 51-417A-12-3,75 | 0 | 2 | 80 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 10 | 3 | 0 | 0 | 60 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | |
107.25 | 51-417A-12-3,75 | 0 | 20 | 98 | VERY DK GRAYISH BROWN | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 96 | 0 | 5 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
109.27 | 51-417A-12-41,127 | 0 | 0 | 95 | ZEOL-BEARING BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 78 | 0 | 2 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | |
109.48 | 51-417A-12-CC,0 | 0 | 0 | 0 | LT BROWN ZEOL-BEARING CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 5 | 7 | 0 | 0 | 78 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
109.48 | 51-417A-12-CC,0 | 0 | 0 | 0 | DK BROWN ZEOL-BEARING CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 8 | 0 | 5 | 20 | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
109.48 | 51-417A-12-CC,0 | 0 | 10 | 90 | WASHED FROM DARK LITH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
113.50 | 51-417A-13-1,50 | 0 | 1 | 99 | ZEOL CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 6 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
116.60 | 51-417A-13-3,60 | 0 | 30 | 70 | DK.BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 35 | 0 | 0 | 40 | 0 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | |
118.12 | 51-417A-13-4,62 | 0 | 40 | 60 | HARD LUMP OF LT BROWN ZEOL CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 40 | 0 | 0 | 40 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
118.22 | 51-417A-13-4,72 | 1 | 25 | 74 | ZEOL CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 2 | 45 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
121.23 | 51-417A-13-CC,0 | 0 | 0 | 0 | 63-149 FROM LT ZEOL CLAY | Dominat lithology; numerical abundance | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 30 | 0 | 0 | 55 | 23 | 23 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
121.23 | 51-417A-13-CC,0 | 0 | 0 | 100 | ZEOL CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
123.56 | 51-417A-14-11,106 | 18 | 80 | 2 | Middle eocene | RAD + SPONGE BEARING ZEOL CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 60 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
123.70 | 51-417A-14-11,120 | 5 | 40 | 55 | Middle eocene | SILIC ZEOL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 60 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
125.02 | 51-417A-14-21,102 | 25 | 30 | 45 | Middle eocene | RAD-BEARING SILIC OOZE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
125.16 | 51-417A-14-21,116 | 10 | 20 | 70 | Middle eocene | RAD-RICH SILIC OOZE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 | 10 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 60 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
125.28 | 51-417A-14-21,128 | 20 | 30 | 50 | Middle eocene | RAD-RICH SILIC OOZE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 10 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 8 | 1 | 0 | 0 | 40 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
125.54 | 51-417A-14-3,4 | 30 | 30 | 45 | Middle eocene | RAD-RICH PINK-ORANGE CLAYEY SILIC OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 38 | 8 | 0 | 20 | 0 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 40 | 0 | 12 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
127.39 | 51-417A-14-4,39 | 85 | 13 | 2 | Middle eocene | RAD SILIC BIOGENIC OOZE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 97 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
131.90 | 51-417A-14-CC,0 | 0 | 0 | 0 | Middle eocene | RAD SAND | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 40 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
131.90 | 51-417A-14-CC,0 | 100 | 50 | 50 | Middle eocene | ZEOL SILT-CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
136.20 | 51-417A-15-31,120 | 10 | 30 | 60 | Middle eocene | ZEOL SILIC OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 15 | 0 | 0 | 0 | 5 | 0 | 4 | 25 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
136.58 | 51-417A-15-4,8 | 10 | 40 | 50 | Middle eocene | DK YELLOW BROWN CLAYEY SILIC OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 10 | 0 | 20 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 1 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
136.75 | 51-417A-15-4,25 | 30 | 40 | 30 | Middle eocene | RAD-RICH CLAYEY FIRM SILIC OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 28 | 15 | 0 | 20 | 0 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.25 | 51-417A-15-4,75 | 5 | 10 | 85 | Middle eocene | REDDISH CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 4 | 0 | 12 | 0 | 0 | 0 | 75 | 0 | 8 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.26 | 51-417A-15-4,76 | 25 | 30 | 45 | Middle eocene | VERY PALE BROWN RAD-RICH CLAYEY SILIC OOZE CLASTS | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.52 | 51-417A-15-CC,0 | 0 | 0 | 0 | Middle eocene | JUST RADS + SPICS | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.52 | 51-417A-15-CC,0 | 10 | 40 | 50 | Middle eocene | RAD-RICH SILIC CLAYEY OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
148.95 | 51-417A-16-51,145 | 15 | 25 | 60 | Middle eocene | FE-MN STAINED ZEOL SILIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 50 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
150.17 | 51-417A-16-61,117 | 20 | 30 | 50 | Middle eocene | DK BROWN CLAYEY SILIC FIRM OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 8 | 0 | 23 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 1 | 0 | 35 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
151.07 | 51-417A-16-CC,0 | 0 | 0 | 0 | Middle eocene | COARSE WASH | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 13 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
151.07 | 51-417A-16-CC,0 | 0 | 0 | 75 | Middle eocene | FERRUG SILIC BROWN CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
151.66 | 51-417A-17-1,66 | 0 | 0 | 0 | Middle eocene | ALTERED VOLC ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
151.67 | 51-417A-17-1,67 | 0 | 0 | 0 | Middle eocene | ALTERED VOLC ASH | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
153.20 | 51-417A-17-CC,0 | 10 | 0 | 0 | Middle eocene | DK BROWN SILIC-BEARING ZEOL SILTY CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 13 | 0 | 0 | 13 | 6 | 2 | 0 | 1 | 0 | 12 | 30 | 0 | 0 | 30 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
153.20 | 51-417A-17-CC,0 | 100 | 40 | 45 | Middle eocene | PINK ZEOL CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 60 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
153.20 | 51-417A-17-CC,0 | 5 | 50 | 50 | Middle eocene | SIEVED FROM PINK + BROWN | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
161.02 | 51-417A-18-1,52 | 0 | 5 | 95 | Middle eocene | REDDISH BROWN PELAGIC CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 90 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
161.04 | 51-417A-18-1,54 | 0 | 10 | 90 | Middle eocene | PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 4 | 4 | 0 | 0 | 81 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
161.11 | 51-417A-18-1,61 | 0 | 5 | 95 | Middle eocene | PALE BROWN CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 90 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
164.35 | 51-417A-18-3,85 | 0 | 20 | 80 | Middle eocene | LT BLUE MOTTLED CLAY (ALT VOLC) | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 | 0 | 3 | 6 | 1 | 0 | 72 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
166.55 | 51-417A-18-5,5 | 0 | 30 | 70 | Middle eocene | FEL-RICH PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 13 | 0 | 0 | 0 | 50 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
166.80 | 51-417A-18-5,30 | 0 | 8 | 92 | Middle eocene | BROWN CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 7 | 4 | 0 | 0 | 83 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
167.38 | 51-417A-18-CC,0 | 0 | 0 | 0 | Middle eocene | CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 5 | 0 | 0 | 5 | 0 | 5 | 5 | 0 | 2 | 70 | 2 | 13 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
167.38 | 51-417A-18-CC,0 | 0 | 0 | 0 | Middle eocene | REDDISH PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
167.38 | 51-417A-18-CC,0 | 0 | 20 | 70 | Middle eocene | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
167.38 | 51-417A-18-CC,0 | 5 | 25 | 80 | Middle eocene | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
170.50 | 51-417A-19-1,50 | 0 | 8 | 92 | Upper cretaceous | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 88 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
170.93 | 51-417A-19-1,93 | 5 | 25 | 70 | Upper cretaceous | VERY DK GRAYISH BROWN PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 25 | 0 | 5 | 0 | 13 | 0 | 0 | 0 | 60 | 0 | 4 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 |
172.64 | 51-417A-19-21,114 | 1 | 15 | 84 | Upper cretaceous | DK GRAYISH BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 2 | 0 | 0 | 80 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
174.30 | 51-417A-19-31,130 | 1 | 10 | 80 | Upper cretaceous | DK BROWN PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 10 | 2 | 0 | 0 | 70 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
174.30 | 51-417A-19-31,130 | 5 | 19 | 85 | Upper cretaceous | DK GRAYISH BROWN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 80 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
178.52 | 51-417A-19-CC,0 | 0 | 0 | 0 | Upper cretaceous | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 18 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 10 | 0 | 0 | 5 | 0 | 20 | 20 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 18 | 0 | 0 | 0 | |
178.52 | 51-417A-19-CC,0 | 0 | 0 | 0 | Upper cretaceous | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 18 | 0 | 5 | 0 | 0 | 5 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
179.85 | 51-417A-20-1,35 | 0 | 20 | 80 | Upper cretaceous | DK GRAY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 8 | 0 | 0 | 60 | 1 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
180.06 | 51-417A-20-1,56 | 0 | 30 | 70 | Upper cretaceous | VERY DK ZEOL CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 25 | 0 | 0 | 50 | 2 | 4 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
180.12 | 51-417A-20-1,62 | 0 | 40 | 60 | Upper cretaceous | BLUE ZEOL CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 40 | 0 | 0 | 40 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 95 | 0 | 0 |
181.87 | 51-417A-20-2,87 | 0 | 20 | 80 | Upper cretaceous | ZEOL-BEARING FERRUG DK BROWN CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 8 | 0 | 0 | 60 | 0 | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
187.18 | 51-417A-20-CC,0 | 0 | 0 | 0 | Upper cretaceous | ZEOL CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 10 | 25 | 0 | 5 | 50 | 2 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 20 | 0 | 15 | 0 | 0 | 0 | 0 |
187.18 | 51-417A-20-CC,0 | 10 | 20 | 70 | Upper cretaceous | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
189.25 | 51-417A-21-1,25 | 0 | 40 | 60 | Upper cretaceous | LT.YELLOW GRITTY ZEOL CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 50 | 3 | 0 | 35 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
191.13 | 51-417A-21-2,63 | 0 | 60 | 40 | Upper cretaceous | ZEOL CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 70 | 1 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
192.35 | 51-417A-21-3,35 | 0 | 0 | 0 | Upper cretaceous | PALE BLUE ZEOL CLAY BLEB | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 55 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
192.60 | 51-417A-21-CC,0 | 0 | 0 | 0 | Upper cretaceous | DK.BROWN ZEOL-RICH CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 4 | 0 | 2 | 15 | 68 | 0 | 0 | 5 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
192.60 | 51-417A-21-CC,0 | 0 | 20 | 80 | Upper cretaceous | WASHED 63-149MICRON SAMPLE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
199.30 | 51-417A-22-1,80 | 0 | 50 | 50 | Upper cretaceous | FE-MN NODULE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
199.57 | 51-417A-22-11,107 | 0 | 0 | 0 | Upper cretaceous | ALT VOLC- CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
199.67 | 51-417A-22-CC,0 | 0 | 0 | 0 | Upper cretaceous | BASALT | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 13 | 10 | 4 | 0 | 60 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 13 | 2 | 0 | 0 | 0 | 0 | 0 |
199.67 | 51-417A-22-CC,0 | 0 | 0 | 0 | Upper cretaceous | BASALT INCLUSIONS COMPARED TO BLUE CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 8 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 |
199.67 | 51-417A-22-CC,0 | 30 | 25 | 40 | Upper cretaceous | ZEOL-BEARING ALT VOLC-RICH CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 |
199.67 | 51-417A-22-CC,0 | 5 | 30 | 70 | Upper cretaceous | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
208.50 | 51-417A-23-1,50 | 0 | 0 | 0 | Upper cretaceous | FEL AND ZEOL RICH SILTY CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 | 13 | 1 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 |
208.80 | 51-417A-23-1,80 | 0 | 40 | 60 | Upper cretaceous | ZEOL CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
209.35 | 51-417A-23-CC,0 | 0 | 0 | 0 | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | ||
209.35 | 51-417A-23-CC,0 | 0 | 0 | 0 | Upper cretaceous | 63-149 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 40 | 0 | 0 | 0 | 13 | 6 | 1 | 0 | 50 | 10 | 2 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 6 | 0 | 25 | 75 | 0 | 0 | 0 | 2 | 0 |
209.35 | 51-417A-23-CC,0 | 0 | 0 | 0 | Upper cretaceous | 63-149MICRONS | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 78 | 0 | 0 | 0 | 0 | 0 |
209.35 | 51-417A-23-CC,0 | 15 | 25 | 60 | MUD IN CC WITH BASALT | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |