van Andel, Tjeerd H; Heath, G Ross (2005): Smear slide analysis of Hole 16-162 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230403
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
Yeats, Robert S; Rodolfo, Kelvin S; Kaneps, Ansis G; Dinkelman, Menno G; Cronan, David S; Charleston, Santiago; Bukry, David; Bennett, Richard H; van Andel, Tjeerd H; Heath, G Ross (1973): Initial Reports of the Deep Sea Drilling Project 16. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XVI, 949 pp, https://doi.org/10.2973/dsdp.proc.16.1973
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 14.869800 * Longitude: -140.043500
Date/Time Start: 1971-03-15T00:00:00 * Date/Time End: 1971-03-15T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 150.10 m
Event(s):
16-162 * Latitude: 14.869800 * Longitude: -140.043500 * Date/Time: 1971-03-15T00:00:00 * Elevation: -4854.0 m * Penetration: 153 m * Recovery: 130.8 m * Location: North Pacific/CONT RISE * Campaign: Leg16 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 17 cores; 153 m cored; 0 m drilled; 85.5 % 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 | Dolomite | Dol | % | Smear slide analysis | ||
10 | Nannofossils | Nannos | % | Smear slide analysis | ||
11 | Foraminifera | Foram | % | Smear slide analysis | ||
12 | Chert | Chert | % | Smear slide analysis | fragments | |
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Minerals, other | Min other | % | Smear slide analysis | ||
17 | Barite | Brt | % | Smear slide analysis | ||
18 | Quartz | Qz | % | Smear slide analysis | ||
19 | Feldspar | Fsp | % | Smear slide analysis | ||
20 | Zeolite | Zeo | % | Smear slide analysis | ||
21 | Biotite | Bt | % | Smear slide analysis | ||
22 | Clay minerals | Clay min | % | Smear slide analysis | ||
23 | Glauconite | Glt | % | Smear slide analysis | ||
24 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
25 | Iron | Fe | % | Smear slide analysis | ||
26 | Pyroxene | Pyrox | % | Smear slide analysis | ||
27 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
28 | Palagonite | Palagonite | % | Smear slide analysis | ||
29 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
5404 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Dol [%] | 10 Nannos [%] | 11 Foram [%] | 12 Chert [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Spiculae [%] | 16 Min other [%] | 17 Brt [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Bt [%] | 22 Clay min [%] | 23 Glt [%] | 24 Py [%] | 25 Fe [%] | 26 Pyrox [%] | 27 Volc glass [%] | 28 Palagonite [%] | 29 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.00 | 16-162-1-0,0 | 0 | 0 | 0 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 32 | 1 | 32 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 32 | 0 | 0 |
0.19 | 16-162-1-1,4 | 0 | 0 | 60 | Lower oligocene | FERRUGINOUS RAD CLAY | Dominat lithology; numerical abundance | 0 | 12 | 0 | 0 | 29 | 1 | 0 | 29 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 29 | 0 | 1 |
0.50 | 16-162-1-1,35 | 0 | 0 | 60 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
0.75 | 16-162-1-1,60 | 0 | 0 | 60 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 35 | 0 | 0 | 35 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 14 | 0 | 14 |
1.25 | 16-162-1-11,110 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
1.97 | 16-162-1-2,32 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
2.45 | 16-162-1-2,80 | 0 | 0 | 60 | Lower oligocene | NANNO RAD MARL | Dominat lithology; numerical abundance | 0 | 35 | 0 | 0 | 35 | 14 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 14 |
3.60 | 16-162-1-3,45 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 |
4.81 | 16-162-1-4,16 | 0 | 0 | 60 | Lower oligocene | RAD CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 33 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 33 | 0 | 33 |
5.05 | 16-162-1-4,40 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 |
5.35 | 16-162-1-4,70 | 0 | 0 | 60 | Lower oligocene | RAD CLAY | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 24 | 0 | 55 |
5.55 | 16-162-1-4,90 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
5.75 | 16-162-1-41,110 | 0 | 0 | 60 | Lower oligocene | FERRUGINOUS RAD CLAY | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 55 |
6.01 | 16-162-1-41,136 | 0 | 0 | 0 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.21 | 16-162-1-5,6 | 0 | 0 | 60 | Lower oligocene | CLAY | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 23 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 55 |
6.51 | 16-162-1-5,36 | 0 | 0 | 1 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
6.63 | 16-162-1-5,48 | 0 | 0 | 60 | Lower oligocene | FERRUGINOUS RAD CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
7.20 | 16-162-1-51,105 | 0 | 0 | 60 | Lower oligocene | MARLY RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 33 |
7.37 | 16-162-1-51,122 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
7.63 | 16-162-1-51,148 | 0 | 0 | 0 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
7.81 | 16-162-1-6,16 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
7.91 | 16-162-1-6,26 | 0 | 0 | 60 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
8.11 | 16-162-1-6,46 | 0 | 0 | 60 | Lower oligocene | NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
8.43 | 16-162-1-6,78 | 0 | 0 | 60 | Lower oligocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 1 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 23 | 0 | 1 | 0 | 55 |
8.57 | 16-162-1-6,92 | 0 | 0 | 35 | Lower oligocene | NANNO RAD CHALK OOZE | Minor lithology; numerical abundance | 0 | 35 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 15 |
8.71 | 16-162-1-61,106 | 0 | 0 | 60 | Lower oligocene | RAD CLAY | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 55 |
8.86 | 16-162-1-61,121 | 0 | 0 | 60 | Lower oligocene | NANNO CHALK OOZE | Minor lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
9.01 | 16-162-1-61,136 | 0 | 0 | 60 | Lower oligocene | RAD CLAY | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 55 |
9.25 | 16-162-1-CC,0 | 0 | 0 | 35 | Lower oligocene | CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 23 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
9.71 | 16-162-2-1,71 | 0 | 0 | 60 | Lower oligocene | NANNO RAD MARL OOZE | Minor lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
10.06 | 16-162-2-11,106 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
10.84 | 16-162-2-2,34 | 0 | 0 | 60 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
10.99 | 16-162-2-2,49 | 0 | 0 | 1 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
11.70 | 16-162-2-21,120 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
12.75 | 16-162-2-3,75 | 0 | 0 | 1 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 |
14.03 | 16-162-2-4,53 | 0 | 0 | 35 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 23 |
14.40 | 16-162-2-4,90 | 0 | 0 | 35 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
14.66 | 16-162-2-41,116 | 0 | 0 | 35 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 23 |
15.16 | 16-162-2-5,16 | 0 | 0 | 35 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 35 | 0 | 0 | 35 | 14 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 14 |
15.83 | 16-162-2-5,83 | 0 | 0 | 60 | Lower oligocene | RAD CLAY | Minor lithology; relative abundance | 0 | 23 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 1 | 55 |
16.97 | 16-162-2-6,47 | 0 | 0 | 60 | Lower oligocene | RAD CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 55 |
17.85 | 16-162-2-61,135 | 0 | 0 | 1 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 |
18.10 | 16-162-2-CC,0 | 0 | 0 | 35 | Lower oligocene | RAD CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 23 | 55 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 1 | 0 | 0 |
18.75 | 16-162-3-1,75 | 0 | 0 | 35 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
19.75 | 16-162-3-2,25 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
20.25 | 16-162-3-2,75 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 23 |
20.67 | 16-162-3-21,117 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 29 | 0 | 0 | 29 | 29 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 |
21.56 | 16-162-3-3,56 | 0 | 0 | 35 | Lower oligocene | RAD NANNO CHALK OOZE | Minor lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 |
21.75 | 16-162-3-3,75 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
22.85 | 16-162-3-4,35 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
23.85 | 16-162-3-41,135 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
24.35 | 16-162-3-5,35 | 0 | 0 | 60 | Lower oligocene | NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 25 | 0 | 0 | 25 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 25 |
25.14 | 16-162-3-51,114 | 0 | 0 | 60 | Lower oligocene | NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 29 | 0 | 0 | 29 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 29 |
25.45 | 16-162-3-51,145 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 1 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 23 |
26.04 | 16-162-3-6,54 | 0 | 0 | 60 | Lower oligocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
26.82 | 16-162-3-61,132 | 0 | 0 | 60 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
27.10 | 16-162-3-CC,0 | 0 | 0 | 1 | Lower oligocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 23 | 39 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
27.34 | 16-162-4-1,19 | 0 | 0 | 60 | Lower oligocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 55 |
27.76 | 16-162-4-1,61 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
28.72 | 16-162-4-2,7 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
29.45 | 16-162-4-2,80 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
29.85 | 16-162-4-21,120 | 0 | 0 | 35 | Lower oligocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
30.68 | 16-162-4-3,53 | 0 | 0 | 0 | Lower oligocene | RAD OOZE | Minor lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 23 |
31.38 | 16-162-4-31,121 | 0 | 0 | 0 | Lower oligocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
31.56 | 16-162-4-31,141 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Minor lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
32.25 | 16-162-4-4,60 | 0 | 0 | 60 | Lower oligocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
33.29 | 16-162-4-5,14 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
33.58 | 16-162-4-5,41 | 0 | 0 | 1 | Lower oligocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 1 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 |
34.95 | 16-162-4-6,30 | 0 | 0 | 60 | Lower oligocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
36.25 | 16-162-4-CC,0 | 0 | 0 | 1 | Upper eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 |
36.85 | 16-162-5-1,85 | 0 | 0 | 60 | Upper eocene | NANNO RAD MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 33 |
37.35 | 16-162-5-11,135 | 0 | 0 | 60 | Upper eocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
38.50 | 16-162-5-21,100 | 0 | 0 | 60 | Upper eocene | RAD CLAY OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
40.40 | 16-162-5-31,140 | 0 | 0 | 60 | Upper eocene | RAD CLAY OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
41.25 | 16-162-5-4,75 | 0 | 0 | 60 | Upper eocene | RAD CLAY OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
42.75 | 16-162-5-5,75 | 0 | 0 | 60 | Upper eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
44.25 | 16-162-5-6,75 | 0 | 0 | 60 | Upper eocene | MARLY RAD OOZE | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
45.10 | 16-162-5-CC,0 | 0 | 0 | 1 | Upper eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
45.13 | 16-162-6-1,13 | 0 | 0 | 35 | Upper eocene | MARLY RAD OOZE | Dominat lithology; numerical abundance | 0 | 26 | 0 | 0 | 26 | 36 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 11 |
46.15 | 16-162-6-11,115 | 0 | 0 | 60 | Upper eocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
46.23 | 16-162-6-11,121 | 0 | 0 | 0 | Upper eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
47.84 | 16-162-6-21,134 | 0 | 0 | 60 | Upper eocene | NANNO RAD MARLY OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
48.75 | 16-162-6-3,75 | 0 | 0 | 60 | Upper eocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 55 |
49.22 | 16-162-6-31,120 | 0 | 0 | 0 | Upper eocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
49.70 | 16-162-6-4,20 | 0 | 0 | 60 | Upper eocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
49.86 | 16-162-6-4,36 | 0 | 0 | 60 | Upper eocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
50.09 | 16-162-6-4,59 | 0 | 0 | 60 | Upper eocene | FERRUGINOUS RAD CLAY OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
51.10 | 16-162-6-CC,0 | 0 | 0 | 1 | Upper eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 23 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
54.75 | 16-162-7-1,75 | 0 | 0 | 35 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 1 | 23 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
54.88 | 16-162-7-1,88 | 0 | 0 | 35 | Middle eocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
59.10 | 16-162-7-4,60 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
60.30 | 16-162-7-5,30 | 0 | 0 | 35 | Middle eocene | RAD OOZE AND VOLCANIC ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
60.60 | 16-162-7-5,60 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
61.23 | 16-162-7-51,121 | 0 | 0 | 10 | Middle eocene | CLAYEY RAD OOZE | relative abundance | 0 | 0 | 0 | 0 | 55 | 1 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
61.88 | 16-162-7-6,38 | 0 | 0 | 35 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
63.10 | 16-162-7-CC,0 | 0 | 0 | 1 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 23 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
63.75 | 16-162-8-1,56 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 1 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
64.19 | 16-162-8-11,100 | 0 | 0 | 1 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 |
64.62 | 16-162-8-11,143 | 0 | 0 | 35 | Middle eocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
64.97 | 16-162-8-2,28 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
65.85 | 16-162-8-21,116 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
66.94 | 16-162-8-3,75 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
67.15 | 16-162-8-3,96 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 |
68.44 | 16-162-8-4,75 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 1 | 55 | 1 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
70.49 | 16-162-8-51,130 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
71.59 | 16-162-8-6,90 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
72.29 | 16-162-8-CC,0 | 0 | 0 | 1 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 1 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
72.92 | 16-162-9-1,92 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 33 |
73.35 | 16-162-9-11,135 | 0 | 0 | 1 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
73.64 | 16-162-9-2,14 | 0 | 0 | 35 | Middle eocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
73.90 | 16-162-9-2,40 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS CLAYEY RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
74.70 | 16-162-9-21,120 | 0 | 0 | 60 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 33 | 1 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 33 |
76.04 | 16-162-9-31,104 | 0 | 0 | 35 | Middle eocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
76.24 | 16-162-9-31,124 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS CLAYEY RAD MARL OOZE | Dominat lithology; relative abundance | 0 | 23 | 1 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
76.60 | 16-162-9-4,10 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
76.72 | 16-162-9-4,22 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
77.80 | 16-162-9-41,130 | 0 | 0 | 35 | Middle eocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
78.17 | 16-162-9-5,17 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
78.40 | 16-162-9-5,40 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS CLAYEY RAD MARL OOZE | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
79.13 | 16-162-9-51,111 | 0 | 0 | 10 | Middle eocene | FERRUGINOUS CLAYEY RAD MARL OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 |
80.50 | 16-162-9-61,100 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
81.10 | 16-162-9-CC,0 | 0 | 0 | 1 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
84.30 | 16-162-10-3,30 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
84.50 | 16-162-10-3,50 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
85.27 | 16-162-10-31,127 | 0 | 0 | 1 | Middle eocene | RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 |
86.42 | 16-162-10-4,92 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 1 | 23 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 55 |
90.10 | 16-162-10-CC,0 | 0 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
91.40 | 16-162-11-11,140 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 33 |
92.02 | 16-162-11-2,52 | 0 | 0 | 1 | Middle eocene | RAD NANNO MARL | Minor lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 |
92.80 | 16-162-11-21,130 | 0 | 0 | 1 | Middle eocene | RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 1 |
93.75 | 16-162-11-3,75 | 0 | 0 | 60 | Middle eocene | RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 1 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
94.24 | 16-162-11-31,124 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
94.27 | 16-162-11-31,127 | 0 | 0 | 10 | Middle eocene | RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
94.84 | 16-162-11-4,34 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
95.40 | 16-162-11-4,90 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
96.60 | 16-162-11-5,60 | 0 | 0 | 35 | Middle eocene | FERRUGINOUS CLAYEY RAD MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
97.00 | 16-162-11-51,100 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
97.12 | 16-162-11-51,112 | 0 | 0 | 35 | Middle eocene | NANNO RAD CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
97.22 | 16-162-11-51,121 | 0 | 0 | 0 | Middle eocene | NANNO RAD CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 |
97.36 | 16-162-11-51,136 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
99.10 | 16-162-11-CC,0 | 0 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
101.25 | 16-162-12-2,75 | 0 | 0 | 35 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
102.75 | 16-162-12-3,75 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
103.22 | 16-162-12-31,121 | 0 | 0 | 1 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
104.90 | 16-162-12-41,140 | 0 | 0 | 35 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
106.15 | 16-162-12-51,115 | 0 | 0 | 35 | Middle eocene | RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
106.22 | 16-162-12-51,121 | 0 | 0 | 0 | Middle eocene | RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
107.30 | 16-162-12-6,80 | 0 | 0 | 35 | Middle eocene | RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
108.10 | 16-162-12-CC,0 | 0 | 0 | 0 | Middle eocene | RAD MARL OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
109.51 | 16-162-13-11,140 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
109.84 | 16-162-13-2,23 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
110.16 | 16-162-13-2,55 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 1 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 33 |
111.61 | 16-162-13-3,50 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
111.66 | 16-162-13-3,55 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
112.97 | 16-162-13-4,36 | 0 | 0 | 35 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
115.99 | 16-162-13-6,38 | 0 | 0 | 60 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 32 | 1 | 0 | 32 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 32 |
116.46 | 16-162-13-6,85 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
117.21 | 16-162-13-CC,0 | 0 | 0 | 1 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
117.44 | 16-162-14-1,25 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
118.19 | 16-162-14-11,100 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 29 | 1 | 0 | 29 | 11 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 29 |
118.97 | 16-162-14-2,28 | 0 | 0 | 60 | Middle eocene | MICRONODULAR DIATOM RAD NANNO MARL OOZE | Minor lithology; numerical abundance | 0 | 25 | 0 | 0 | 25 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 |
119.19 | 16-162-14-2,50 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 33 | 0 | 0 | 33 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
121.39 | 16-162-14-31,120 | 0 | 0 | 60 | Middle eocene | RAD NANNO CLAYEY MARL OOZE | Dominat lithology; numerical abundance | 1 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 33 |
121.41 | 16-162-14-31,120 | 0 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
122.94 | 16-162-14-41,125 | 0 | 0 | 35 | Middle eocene | NANNO RAD CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
125.02 | 16-162-14-6,33 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 32 | 1 | 0 | 32 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 32 |
125.32 | 16-162-14-6,63 | 0 | 0 | 35 | Middle eocene | RAD NANNO MARL OOZE | Minor lithology; numerical abundance | 1 | 35 | 1 | 0 | 35 | 14 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 14 |
127.50 | 16-162-15-11,130 | 0 | 0 | 60 | Middle eocene | RAD NANNO CLAYEY MARL | Dominat lithology; numerical abundance | 0 | 32 | 1 | 0 | 32 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 32 |
128.52 | 16-162-15-2,82 | 0 | 0 | 35 | Middle eocene | RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 55 | 1 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 23 |
130.43 | 16-162-15-31,121 | 0 | 0 | 0 | Middle eocene | RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
131.22 | 16-162-15-4,52 | 0 | 0 | 0 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
131.50 | 16-162-15-4,80 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 0 | 32 | 0 | 0 | 32 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 32 |
132.08 | 16-162-15-41,138 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; numerical abundance | 1 | 32 | 1 | 0 | 32 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 32 |
133.44 | 16-162-15-51,122 | 0 | 0 | 0 | Middle eocene | CLAYEY RAD NANNO MARL OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
133.98 | 16-162-15-6,28 | 0 | 0 | 35 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 1 |
134.29 | 16-162-15-6,59 | 0 | 0 | 60 | Middle eocene | RAD NANNO CLAYEY MARL OOZE | Dominat lithology; numerical abundance | 1 | 33 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 33 |
135.30 | 16-162-15-CC,0 | 0 | 0 | 1 | Middle eocene | RAD NANNO CLAYEY CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
135.92 | 16-162-16-1,92 | 0 | 0 | 35 | Middle eocene | RAD NANNO MARL OOZE | Minor lithology; numerical abundance | 0 | 35 | 0 | 0 | 35 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 15 |
136.12 | 16-162-16-11,112 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
136.46 | 16-162-16-11,145 | 0 | 0 | 0 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.50 | 16-162-16-21,100 | 0 | 0 | 60 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
138.00 | 16-162-16-3,0 | 0 | 0 | 1 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 1 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
139.60 | 16-162-16-CC,0 | 0 | 0 | 1 | Middle eocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 |
144.62 | 16-162-17-1,62 | 0 | 0 | 60 | Middle eocene | ZEOLITE-BEARING FERRUGINOUS CLAY | Dominat lithology; relative abundance | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
144.75 | 16-162-17-1,75 | 0 | 0 | 60 | Middle eocene | CLAYEY NANNO MARL | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
144.76 | 16-162-17-1,75 | 0 | 0 | 35 | Middle eocene | CLAYEY NANNO MARL | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 15 | 35 | 0 |
144.77 | 16-162-17-1,77 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS CLAYEY NANNO MARL | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 55 |
146.35 | 16-162-17-2,85 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
146.56 | 16-162-17-21,104 | 0 | 0 | 0 | Middle eocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 55 | 55 | 0 |
147.63 | 16-162-17-3,61 | 0 | 0 | 0 | Middle eocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 56 | 55 | 0 |
149.80 | 16-162-17-41,130 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 29 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 29 |
149.98 | 16-162-17-41,148 | 0 | 0 | 60 | Middle eocene | FERRUGINOUS NANNO MARL | Minor lithology; relative abundance | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
150.10 | 16-162-17-CC,0 | 0 | 0 | 60 | Middle eocene | BASALT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 1 | 14 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 34 | 14 |