Tucholke, Brian E; Vogt, Peter R (2005): Smear slide analysis of Hole 43-385 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230721
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
DSDP (1989): Data from the Deep Sea Drilling Project. Sediment, hard rock and reference files. National Geophysical Data Center, National Environmental Satellite, Data and Information Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1, CD-ROM
McCave, I Nick; Demars, Kenneth R; Kendrick, J W; Okada, Hisatake; McNulty, C L; Kaneps, Ansis G; Galehouse, J S; Houghton, R L; Rothe, Peter; Murdmaa, Ivar O; Tucholke, Brian E; Vogt, Peter R (1979): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XLIII, 1115 pp, https://doi.org/10.2973/dsdp.proc.43.1979
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 37.369500 * Longitude: -60.157500
Date/Time Start: 1975-07-18T00:00:00 * Date/Time End: 1975-07-18T00:00:00
Minimum DEPTH, sediment/rock: 23.35 m * Maximum DEPTH, sediment/rock: 308.78 m
Event(s):
43-385 * Latitude: 37.369500 * Longitude: -60.157500 * Date/Time: 1975-07-18T00:00:00 * Elevation: -4936.0 m * Penetration: 392.9 m * Recovery: 64 m * Location: North Atlantic/SEAMOUNT * Campaign: Leg43 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 218.2 m cored; 9.5 m drilled; 29.3 % 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 | Nannofossils | Nannos | % | Smear slide analysis | ||
11 | Foraminifera | Foram | % | Smear slide analysis | ||
12 | Lamellibranchiata | Lamellibranchiata | % | Smear slide analysis | ||
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Minerals, other | Min other | % | Smear slide analysis | ||
18 | Siderite | Sd | % | Smear slide analysis | ||
19 | Barite | Brt | % | Smear slide analysis | ||
20 | Quartz | Qz | % | Smear slide analysis | ||
21 | Feldspar | Fsp | % | Smear slide analysis | ||
22 | Zeolite | Zeo | % | Smear slide analysis | ||
23 | Mica | Mica | % | Smear slide analysis | ||
24 | Biotite | Bt | % | Smear slide analysis | ||
25 | Clay minerals | Clay min | % | Smear slide analysis | ||
26 | Glauconite | Glt | % | Smear slide analysis | ||
27 | Opaque minerals | Opaque | % | Smear slide analysis | ||
28 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
29 | Iron | Fe | % | Smear slide analysis | ||
30 | Heavy minerals | HM | % | Smear slide analysis | ||
31 | Rutile | Rt | % | Smear slide analysis | ||
32 | Apatite | Ap | % | Smear slide analysis | ||
33 | Epidote | Ep | % | Smear slide analysis | ||
34 | Amphibole | Amp | % | Smear slide analysis | ||
35 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
36 | Palagonite | Palagonite | % | Smear slide analysis | ||
37 | Manganese | Mn | % | Smear slide analysis | ||
38 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus | |
39 | Amorphics | Amorphics | % | Smear slide analysis | amorphous oxide |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4705 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 Nannos [%] | 11 Foram [%] | 12 Lamellibranchiata [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Silicoflag [%] | 16 Spiculae [%] | 17 Min other [%] | 18 Sd [%] | 19 Brt [%] | 20 Qz [%] | 21 Fsp [%] | 22 Zeo [%] | 23 Mica [%] | 24 Bt [%] | 25 Clay min [%] | 26 Glt [%] | 27 Opaque [%] | 28 Py [%] | 29 Fe [%] | 30 HM [%] | 31 Rt [%] | 32 Ap [%] | 33 Ep [%] | 34 Amp [%] | 35 Volc glass [%] | 36 Palagonite [%] | 37 Mn [%] | 38 Terr [%] | 39 Amorphics [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
23.35 | 43-385-1-11,105 | 20 | 40 | 40 | Pleistocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 22 | 15 | 25 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 10 | 1 | 2 | 1 | 0 | 25 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 60 | 0 |
23.49 | 43-385-1-11,119 | 1 | 27 | 72 | Pleistocene | SILTY CLAY | Minor lithology; relative abundance | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 2 | 0 | 2 | 0 | 72 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 100 | 5 |
23.60 | 43-385-1-11,130 | 0 | 5 | 95 | Pleistocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 2 | 2 | 0 | 95 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 100 | 0 |
24.16 | 43-385-1-2,36 | 10 | 40 | 50 | Pleistocene | PALAGONITIC SILTY CLAY | Minor lithology; relative abundance | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 50 | 2 | 100 | 0 |
24.55 | 43-385-1-2,75 | 0 | 5 | 95 | Pleistocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 95 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 100 | 0 |
26.05 | 43-385-1-3,75 | 0 | 5 | 95 | Pleistocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 95 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 |
26.60 | 43-385-1-31,130 | 60 | 30 | 10 | Pleistocene | ZEOLITE-PALAGONITE SILTY SAND | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 35 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 55 | 0 | 100 | 0 |
26.68 | 43-385-1-31,138 | 0 | 2 | 98 | Pleistocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 98 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
27.55 | 43-385-1-4,75 | 0 | 5 | 95 | Pleistocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 95 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 100 | 0 |
61.60 | 43-385-2-1,75 | 0 | 5 | 95 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 |
62.53 | 43-385-2-2,18 | 0 | 13 | 87 | Upper oligocene | CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 87 | 0 | 8 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 97 | 0 |
63.10 | 43-385-2-2,75 | 1 | 10 | 90 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 3 | 2 | 2 | 2 | 0 | 90 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 96 | 0 |
64.60 | 43-385-2-3,75 | 0 | 7 | 93 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 2 | 0 | 93 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 97 | 0 |
65.60 | 43-385-2-4,25 | 0 | 7 | 93 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 93 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 94 | 0 |
66.10 | 43-385-2-4,75 | 0 | 5 | 95 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 97 | 0 |
67.60 | 43-385-2-5,75 | 3 | 6 | 91 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 92 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 94 | 0 |
68.85 | 43-385-2-6,50 | 0 | 6 | 94 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 4 | 1 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 94 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 |
69.10 | 43-385-2-6,75 | 0 | 1 | 99 | Upper oligocene | CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 88 | 10 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 100 | 0 |
69.70 | 43-385-2-61,135 | 5 | 10 | 85 | Upper oligocene | CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 2 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 87 | 7 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 88 | 0 |
98.90 | 43-385-3-1,10 | 0 | 3 | 97 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 97 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 100 | 0 |
99.16 | 43-385-3-1,36 | 15 | 10 | 75 | Upper oligocene | GLAUCONITIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 74 | 23 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 |
99.55 | 43-385-3-1,75 | 0 | 2 | 98 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 98 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 100 | 0 |
101.05 | 43-385-3-2,75 | 0 | 4 | 96 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 96 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 100 | 0 |
101.41 | 43-385-3-21,111 | 0 | 2 | 98 | Upper oligocene | CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 98 | 2 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 100 | 0 |
101.98 | 43-385-3-3,18 | 1 | 3 | 97 | Upper oligocene | CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 97 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 97 | 0 |
102.55 | 43-385-3-3,75 | 0 | 2 | 98 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 98 | 2 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 |
103.27 | 43-385-3-31,147 | 3 | 10 | 87 | Upper oligocene | CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 2 | 2 | 2 | 0 | 0 | 0 | 1 | 2 | 0 | 2 | 0 | 87 | 7 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 90 | 0 |
104.05 | 43-385-3-4,75 | 10 | 15 | 75 | Upper oligocene | GLAUCONITIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 75 | 20 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 77 | 0 |
105.55 | 43-385-3-5,75 | 0 | 2 | 98 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 98 | 2 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 100 | 0 |
107.05 | 43-385-3-6,75 | 0 | 2 | 98 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 98 | 2 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 100 | 0 |
137.58 | 43-385-4-11,108 | 1 | 8 | 91 | Middle eocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 3 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 91 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 97 | 0 |
137.62 | 43-385-4-11,112 | 5 | 37 | 58 | Middle eocene | RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 40 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 58 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 58 | 0 |
137.73 | 43-385-4-11,123 | 2 | 41 | 57 | Middle eocene | RADIOLARIAN CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 40 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 57 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 57 | 0 |
137.79 | 43-385-4-11,129 | 2 | 30 | 68 | Middle eocene | RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 2 | 2 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 68 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 61 | 0 |
137.91 | 43-385-4-11,141 | 5 | 38 | 57 | Middle eocene | RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 40 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 57 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 57 | 0 |
138.20 | 43-385-4-2,20 | 1 | 65 | 44 | Middle eocene | CLAYEY RADIOLARIAN OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 50 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 44 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 44 | 0 |
138.75 | 43-385-4-2,75 | 1 | 46 | 54 | Middle eocene | RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 40 | 5 | 2 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 54 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 55 | 0 |
139.30 | 43-385-4-21,130 | 5 | 40 | 55 | Middle eocene | CLAYEY RADIOLARIAN OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 45 | 5 | 2 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 |
140.25 | 43-385-4-3,75 | 2 | 56 | 42 | Middle eocene | CLAYEY RADIOLARIAN OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 42 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 42 | 0 |
140.50 | 43-385-4-31,100 | 1 | 44 | 55 | Middle eocene | CLAYEY RADIOLARIAN OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 45 | 5 | 2 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 |
140.65 | 43-385-4-31,115 | 5 | 40 | 55 | Middle eocene | RADIOLARIAN CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 40 | 5 | 2 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 |
140.75 | 43-385-4-31,125 | 1 | 35 | 64 | Middle eocene | RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 5 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 64 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 65 | 0 |
147.00 | 43-385-5-1,90 | 4 | 66 | 30 | Lower eocene | RADIOLARIAN OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 69 | 1 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 30 | 0 |
147.50 | 43-385-5-11,140 | 2 | 48 | 50 | Lower eocene | RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 40 | 5 | 2 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 |
148.35 | 43-385-5-2,75 | 4 | 32 | 64 | Lower eocene | RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 35 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 64 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 64 | 0 |
148.50 | 43-385-5-2,90 | 5 | 25 | 70 | Lower eocene | RADIOLARIAN CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 4 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 |
149.85 | 43-385-5-3,75 | 1 | 29 | 70 | Lower eocene | RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 |
151.35 | 43-385-5-4,75 | 5 | 35 | 60 | Lower eocene | RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 39 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 60 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 60 | 0 |
155.61 | 43-385-6-CC,1 | 1 | 74 | 25 | Lower eocene | DIATOM-RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 20 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 25 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 25 | 0 |
155.63 | 43-385-6-CC,3 | 1 | 35 | 65 | Lower eocene | DIATOMACEOUS-RADIOLARIAN CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 5 | 2 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 65 | 0 |
165.16 | 43-385-7-CC,6 | 0 | 30 | 70 | ZEOLITIC SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 70 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 100 | 0 | |
165.20 | 43-385-7-CC,10 | 3 | 37 | 60 | ZEOLITIC SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 60 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 100 | 0 | |
165.25 | 43-385-7-CC,15 | 0 | 40 | 30 | METALLIFEROUS ZEOLITIC SILTY CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 30 | 0 | 0 | |
165.25 | 43-385-7-CC,15 | 1 | 70 | 60 | ZEOLITIC CLAYEY SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | |
175.61 | 43-385-8-11,101 | 0 | 40 | 60 | ZEOLITIC SILTY CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 60 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
175.80 | 43-385-8-11,120 | 0 | 50 | 50 | ZEOLITIC SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 50 | 0 | 0 | 50 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | |
175.93 | 43-385-8-11,133 | 1 | 60 | 40 | ZEOLITIC CLAYEY SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | |
181.80 | 43-385-8-51,120 | 0 | 35 | 65 | ZEOLITIC (SILTY) CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 35 | 0 | 0 | 65 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | |
184.85 | 43-385-9-1,75 | 5 | 55 | 40 | ZEOLITIC CLAYEY SILT | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | |
185.10 | 43-385-9-11,100 | 1 | 70 | 30 | ZEOLITIC CLAYEY SILT | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 70 | 0 | 0 | 30 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | |
194.49 | 43-385-10-11,109 | 3 | 67 | 30 | ZEOLITIC CLAYEY SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | |
194.57 | 43-385-10-11,117 | 0 | 15 | 85 | CLAY | Dominat lithology; relative abundance | 1 | 2 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 85 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 100 | 0 | |
194.60 | 43-385-10-11,120 | 5 | 15 | 80 | ZEOLITIC CLAY | Dominat lithology; relative abundance | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 20 | 0 | 0 | 80 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | |
203.60 | 43-385-11-1,60 | 0 | 11 | 89 | Lower paleocene | CLAY | Dominat lithology; relative abundance | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 89 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 100 | 0 |
203.70 | 43-385-11-1,70 | 2 | 15 | 83 | Lower paleocene | CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
204.20 | 43-385-11-11,120 | 3 | 17 | 80 | Lower paleocene | ZEOLITIC CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 15 | 2 | 0 | 83 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
205.50 | 43-385-11-21,100 | 0 | 2 | 98 | Lower paleocene | CLAY | Dominat lithology; relative abundance | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 2 | 95 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 100 | 0 |
205.83 | 43-385-11-21,133 | 1 | 39 | 60 | Lower paleocene | ZEOLITIC MARLY CLAY | Minor lithology; relative abundance | 35 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 2 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
205.96 | 43-385-11-21,146 | 2 | 38 | 60 | Lower paleocene | MARLY OOZE | Minor lithology; relative abundance | 28 | 12 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 2 | 0 | 50 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
205.99 | 43-385-11-21,149 | 15 | 25 | 60 | Lower paleocene | MARLY FORAM OOZE | Minor lithology; relative abundance | 23 | 8 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
213.32 | 43-385-12-1,82 | 1 | 39 | 60 | Upper cretaceous | ZEOLITIC SILTY CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 2 | 59 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
213.35 | 43-385-12-1,85 | 0 | 0 | 0 | Upper cretaceous | CLAY | Minor lithology; relative abundance | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 94 | 1 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 |
213.44 | 43-385-12-1,94 | 0 | 50 | 50 | Upper cretaceous | NANNO OOZE | Minor lithology; relative abundance | 2 | 70 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 32 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
213.70 | 43-385-12-11,120 | 0 | 30 | 70 | Upper cretaceous | MARLY NANNO OOZE | Dominat lithology; relative abundance | 2 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
214.02 | 43-385-12-2,2 | 0 | 70 | 30 | Upper cretaceous | NANNO OOZE | Dominat lithology; relative abundance | 2 | 90 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 10 | 0 |
214.22 | 43-385-12-2,22 | 0 | 55 | 45 | Upper cretaceous | MARLY NANNO OOZE | Dominat lithology; relative abundance | 1 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 40 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
214.75 | 43-385-12-2,75 | 0 | 2 | 98 | Upper cretaceous | MARLY NANNO OOZE | Dominat lithology; relative abundance | 2 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 50 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 52 | 0 |
232.10 | 43-385-13-1,50 | 3 | 37 | 60 | Maestrichtian | CALCAREOUS SILTY CLAY | Minor lithology; relative abundance | 6 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 1 | 2 | 10 | 0 | 0 | 0 | 59 | 0 | 0 | 0 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
232.35 | 43-385-13-1,75 | 0 | 20 | 80 | Maestrichtian | CLAY (MARLY NANNO OOZE ?) | Dominat lithology; relative abundance | 1 | 24 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 75 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 76 | 0 |
232.54 | 43-385-13-1,94 | 0 | 25 | 75 | Maestrichtian | MARLY NANNO OOZE | Minor lithology; relative abundance | 1 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 69 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 70 | 0 |
233.85 | 43-385-13-2,75 | 0 | 70 | 30 | Maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 2 | 79 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 20 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 21 | 0 |
234.28 | 43-385-13-21,118 | 0 | 40 | 60 | Maestrichtian | MARLY NANNO OOZE | Minor lithology; relative abundance | 2 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 60 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 |
234.80 | 43-385-13-3,20 | 0 | 1 | 99 | Maestrichtian | CLAY | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 100 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 100 | 0 |
235.50 | 43-385-13-3,90 | 0 | 75 | 25 | Maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
236.85 | 43-385-13-4,75 | 0 | 50 | 50 | Maestrichtian | MARLY NANNO OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 45 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 45 | 0 |
237.15 | 43-385-13-41,105 | 0 | 0 | 0 | Maestrichtian | LIMESTONE | Minor lithology; numerical abundance | 100 | 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 | 100 | 0 |
237.42 | 43-385-13-41,132 | 0 | 5 | 95 | Maestrichtian | CLAY | Minor lithology; relative abundance | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 97 | 0 |
237.50 | 43-385-13-41,140 | 0 | 70 | 30 | Maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 2 | 80 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
251.35 | 43-385-14-1,75 | 0 | 10 | 90 | CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 90 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 0 | 0 | |
251.65 | 43-385-14-11,105 | 1 | 27 | 73 | VITRIC SILTY CLAY | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 17 | 0 | 0 | 0 | 1 | 1 | 2 | 16 | 50 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 4 | 4 | 2 | 0 | 0 | 0 | 0 | |
251.66 | 43-385-14-11,106 | 10 | 70 | 20 | VITRIC SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 100 | 0 | |
252.40 | 43-385-14-2,30 | 5 | 30 | 65 | VITRIC SILTY CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 65 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | |
252.85 | 43-385-14-2,75 | 1 | 30 | 70 | VITRIC SILTY CLAY | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | |
254.10 | 43-385-14-3,50 | 1 | 30 | 70 | VITRIC SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 29 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | |
254.37 | 43-385-14-3,77 | 1 | 25 | 75 | VITRIC SILTY CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | |
270.06 | 43-385-15-1,46 | 5 | 25 | 70 | Upper cretaceous | VITRIC SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 19 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 70 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
270.12 | 43-385-15-1,52 | 25 | 45 | 30 | Upper cretaceous | VITRIC MUD | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 30 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 |
270.14 | 43-385-15-1,54 | 1 | 10 | 90 | Upper cretaceous | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 90 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 |
270.60 | 43-385-15-11,100 | 0 | 10 | 90 | Upper cretaceous | CLAY | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 |
270.80 | 43-385-15-11,120 | 0 | 0 | 0 | Upper cretaceous | MANGANESE OXIDES AND CLAY | 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 |
280.26 | 43-385-16-11,136 | 0 | 0 | 100 | CLAY ? | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 100 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
280.29 | 43-385-16-11,139 | 0 | 17 | 83 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 83 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 100 | 0 | |
280.50 | 43-385-16-2,10 | 5 | 75 | 20 | ZEOLITIC VITRIC SILT | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 25 | 0 | 0 | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
280.56 | 43-385-16-2,16 | 10 | 60 | 30 | FERRUGINOUS VITRIC CLAYEY SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 30 | 0 | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 100 | 0 | |
280.80 | 43-385-16-2,40 | 1 | 10 | 90 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 90 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
281.01 | 43-385-16-2,61 | 10 | 80 | 10 | VITRIC SILT | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 87 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
281.09 | 43-385-16-2,69 | 10 | 13 | 77 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 77 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | |
281.26 | 43-385-16-2,86 | 20 | 20 | 60 | SILTY CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 22 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 13 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 100 | 0 | |
281.37 | 43-385-16-2,97 | 20 | 70 | 10 | FERRUGINOUS SANDY SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 0 | 0 | 25 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | |
281.44 | 43-385-16-21,104 | 20 | 25 | 55 | FERRUGINOUS SILTY CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 55 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | |
281.70 | 43-385-16-21,130 | 25 | 25 | 50 | VITRIC SILTY CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 100 | 0 | |
281.77 | 43-385-16-21,137 | 30 | 40 | 30 | VITRIC MUD | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | |
282.07 | 43-385-16-3,17 | 20 | 20 | 60 | VITRIC SANDY CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 60 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | |
282.09 | 43-385-16-3,19 | 0 | 100 | 0 | FERRUGINOUS VITRIC SILT | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | |
282.11 | 43-385-16-3,21 | 40 | 45 | 15 | VITRIC SILT | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 100 | 0 | |
282.12 | 43-385-16-3,22 | 45 | 45 | 10 | FERRUGINOUS VITRIC SILTY SAND | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 74 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | |
282.14 | 43-385-16-3,24 | 0 | 0 | 0 | CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 8 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
282.40 | 43-385-16-3,50 | 0 | 10 | 90 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 90 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
282.61 | 43-385-16-3,71 | 25 | 75 | 0 | FERRUGINOUS VITRIC SANDY SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | |
283.26 | 43-385-16-31,136 | 20 | 20 | 60 | VITRIC FERRUGINOUS SILTY CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 100 | 0 | |
283.29 | 43-385-16-31,139 | 15 | 15 | 70 | FERRUGINOUS SILTY CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | |
283.33 | 43-385-16-31,143 | 15 | 65 | 20 | VITRIC CLAYEY SILT | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 58 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 10 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
283.36 | 43-385-16-31,146 | 40 | 45 | 15 | VITRIC SILT | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 100 | 0 | |
308.76 | 43-385-19-11,136 | 0 | 26 | 74 | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 74 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 100 | 0 | |
308.78 | 43-385-19-11,138 | 35 | 35 | 30 | CLAYEY SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 30 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 100 | 0 |