van Andel, Tjeerd H; Heath, G Ross (2005): Smear slide analysis of Hole 16-160 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230400
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: 11.704500 * Longitude: -130.880200
Date/Time Start: 1971-03-05T00:00:00 * Date/Time End: 1971-03-05T00:00:00
Minimum DEPTH, sediment/rock: 0.71 m * Maximum DEPTH, sediment/rock: 109.60 m
Event(s):
16-160 * Latitude: 11.704500 * Longitude: -130.880200 * Date/Time: 1971-03-05T00:00:00 * Elevation: -4940.0 m * Penetration: 114 m * Recovery: 94.9 m * Location: North Pacific/CONT RISE * Campaign: Leg16 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 14 cores; 114 m cored; 0 m drilled; 83.2 % 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 | Nannofossils | Nannos | % | Smear slide analysis | ||
10 | Foraminifera | Foram | % | Smear slide analysis | ||
11 | Calcareous spicules | Calc spic | % | Smear slide analysis | ||
12 | Radiolarians | Rad | % | Smear slide analysis | ||
13 | Diatoms | Diatoms | % | Smear slide analysis | ||
14 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Quartz | Qz | % | Smear slide analysis | ||
17 | Feldspar | Fsp | % | Smear slide analysis | ||
18 | Zeolite | Zeo | % | Smear slide analysis | ||
19 | Iron | Fe | % | Smear slide analysis | ||
20 | Zircon | Zrn | % | Smear slide analysis | ||
21 | Pyroxene | Pyrox | % | Smear slide analysis | ||
22 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
23 | Palagonite | Palagonite | % | Smear slide analysis | ||
24 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1851 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Nannos [%] | 10 Foram [%] | 11 Calc spic [%] | 12 Rad [%] | 13 Diatoms [%] | 14 Silicoflag [%] | 15 Spiculae [%] | 16 Qz [%] | 17 Fsp [%] | 18 Zeo [%] | 19 Fe [%] | 20 Zrn [%] | 21 Pyrox [%] | 22 Volc glass [%] | 23 Palagonite [%] | 24 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.71 | 16-160-1-1,71 | 0 | 0 | 60 | Pleistocene | ZEOLITIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 1 | 0 | 55 |
0.80 | 16-160-1-1,80 | 0 | 0 | 60 | Pleistocene | ZEOLITIC MICRONODULE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 |
1.98 | 16-160-1-2,48 | 0 | 0 | 60 | Pleistocene | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 1 | 0 | 55 |
2.57 | 16-160-1-21,107 | 0 | 0 | 60 | Pleistocene | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 |
3.29 | 16-160-1-3,29 | 0 | 0 | 60 | Pleistocene | MICRONODULE ZEOLITE RADIOLARIAN CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 25 | 25 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 25 |
3.80 | 16-160-1-3,80 | 0 | 0 | 60 | Pleistocene | MICRONODULE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 1 | 0 | 55 |
4.60 | 16-160-1-CC,0 | 0 | 0 | 60 | Pleistocene | ZEOLITIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 |
9.80 | 16-160-2-1,80 | 0 | 0 | 60 | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 1 | 0 | 55 | |
11.31 | 16-160-2-2,81 | 0 | 0 | 60 | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 | |
12.50 | 16-160-2-3,50 | 0 | 0 | 60 | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 | |
12.80 | 16-160-2-3,80 | 0 | 0 | 60 | ZEOLITE MICRONODULE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 | |
13.91 | 16-160-2-4,41 | 0 | 0 | 0 | ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 1 | 0 | 23 | |
15.50 | 16-160-2-5,50 | 0 | 0 | 0 | MOCRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 | |
16.60 | 16-160-2-CC,0 | 0 | 0 | 0 | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 1 | 55 | |
18.86 | 16-160-3-1,86 | 0 | 0 | 0 | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 | |
19.10 | 16-160-3-11,110 | 0 | 0 | 60 | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 | |
20.30 | 16-160-3-2,80 | 0 | 0 | 60 | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 | |
23.30 | 16-160-3-4,80 | 0 | 0 | 60 | Lower miocene | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 |
24.80 | 16-160-3-5,80 | 0 | 0 | 60 | Lower miocene | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 |
26.01 | 16-160-3-6,51 | 0 | 0 | 60 | Lower miocene | MICRONODULE ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 55 |
26.55 | 16-160-3-61,105 | 0 | 0 | 60 | Lower miocene | ZEOLITIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 23 | 0 | 1 | 0 | 0 | 0 | 23 |
27.10 | 16-160-3-CC,0 | 0 | 0 | 60 | Lower miocene | MICRONODULE BEARING CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 23 |
27.92 | 16-160-4-1,92 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 56 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 23 |
28.23 | 16-160-4-11,123 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
29.30 | 16-160-4-2,80 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 60 | 0 | 0 | 13 | 1 | 0 | 13 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 |
30.85 | 16-160-4-3,85 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 56 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
32.56 | 16-160-4-41,106 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 56 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
33.90 | 16-160-4-5,90 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 1 | 23 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
36.70 | 16-160-5-1,70 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 23 |
38.30 | 16-160-5-2,80 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
39.80 | 16-160-5-3,80 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
41.30 | 16-160-5-4,80 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
45.47 | 16-160-6-1,47 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
45.80 | 16-160-6-1,80 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
47.08 | 16-160-6-2,58 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
47.20 | 16-160-6-2,70 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
48.02 | 16-160-6-3,2 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 56 | 0 | 0 | 23 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
48.50 | 16-160-6-3,50 | 0 | 0 | 0 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
51.80 | 16-160-6-5,80 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
53.20 | 16-160-6-6,70 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
55.40 | 16-160-7-11,140 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
56.20 | 16-160-7-2,70 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 |
56.50 | 16-160-7-21,100 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
57.80 | 16-160-7-3,80 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
59.30 | 16-160-7-4,80 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
59.34 | 16-160-7-4,84 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 12 | 47 | 0 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 |
60.65 | 16-160-7-5,65 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
60.77 | 16-160-7-5,77 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
62.64 | 16-160-7-61,114 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
63.10 | 16-160-7-CC,0 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
63.80 | 16-160-8-1,80 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
65.30 | 16-160-8-2,80 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 |
68.30 | 16-160-8-4,80 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
73.18 | 16-160-9-11,118 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 23 |
73.18 | 16-160-9-11,118 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
75.83 | 16-160-9-3,83 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 23 |
80.30 | 16-160-9-6,80 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
81.49 | 16-160-10-1,49 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 23 |
82.29 | 16-160-10-11,129 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 23 |
83.18 | 16-160-10-2,68 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
84.79 | 16-160-10-3,79 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
86.30 | 16-160-10-4,80 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 23 |
87.80 | 16-160-10-5,80 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
89.50 | 16-160-10-61,100 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
89.96 | 16-160-10-61,146 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
90.80 | 16-160-11-1,80 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 |
92.30 | 16-160-11-2,80 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
93.80 | 16-160-11-3,80 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
95.30 | 16-160-11-4,80 | 0 | 0 | 35 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
96.70 | 16-160-11-5,70 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
98.20 | 16-160-11-6,70 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
99.10 | 16-160-11-CC,0 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
99.80 | 16-160-12-1,80 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
101.30 | 16-160-12-2,80 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
102.80 | 16-160-12-3,80 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
103.08 | 16-160-12-31,108 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
104.30 | 16-160-12-4,80 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
107.30 | 16-160-12-6,80 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
107.90 | 16-160-12-61,140 | 0 | 0 | 35 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
109.36 | 16-160-13-11,136 | 0 | 0 | 35 | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | |
109.60 | 16-160-13-CC,0 | 0 | 0 | 0 | RED MARL OOZE | Dominat lithology; numerical abundance | 29 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 0 | 1 | 0 | 29 | 29 |