McManus, Dean A; Burns, Robert E (2005): Smear slide analysis of Hole 5-36 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230771
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
Milow, E Dean; Goll, Robert M; Olsson, Richard K; von der Borch, Christopher C; Vallier, Tracy L; Weser, Oscar E; Burns, Robert E; McManus, Dean A (1970): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, V, 827 pp, https://doi.org/10.2973/dsdp.proc.5.1970
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 40.984700 * Longitude: -130.109700
Date/Time Start: 1969-05-06T00:00:00 * Date/Time End: 1969-05-06T00:00:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 116.20 m
Event(s):
5-36 * Latitude: 40.984700 * Longitude: -130.109700 * Date/Time: 1969-05-06T00:00:00 * Elevation: -3273.0 m * Penetration: 115.5 m * Recovery: 102.7 m * Location: North Pacific/RIDGE * Campaign: Leg5 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 104.5 m cored; 0 m drilled; 98.3 % 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 | Dolomite | Dol | % | Smear slide analysis | ||
11 | Nannofossils | Nannos | % | Smear slide analysis | ||
12 | Foraminifera | Foram | % | Smear slide analysis | ||
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 | Quartz | Qz | % | Smear slide analysis | ||
18 | Feldspar | Fsp | % | Smear slide analysis | ||
19 | Zeolite | Zeo | % | Smear slide analysis | ||
20 | Clay minerals | Clay min | % | Smear slide analysis | ||
21 | Opaque minerals | Opaque | % | Smear slide analysis | ||
22 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
23 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
24 | Palagonite | Palagonite | % | Smear slide analysis | ||
25 | Fragments | Fragm | % | Smear slide analysis | calcareous material | |
26 | Pumice | Pumice | % | Smear slide analysis | ||
27 | Manganese | Mn | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2444 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Carb [%] | 10 Dol [%] | 11 Nannos [%] | 12 Foram [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Spiculae [%] | 16 Min other [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Clay min [%] | 21 Opaque [%] | 22 Py [%] | 23 Volc glass [%] | 24 Palagonite [%] | 25 Fragm [%] | 26 Pumice [%] | 27 Mn [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.05 | 5-36-1-1,5 | 10 | 10 | 80 | Pleistocene | FORAM MARL MUD | Minor lithology; relative abundance | 0 | 0 | 2 | 30 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 70 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
0.27 | 5-36-1-1,27 | 5 | 65 | 10 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 55 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
0.40 | 5-36-1-1,40 | 10 | 20 | 70 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
0.64 | 5-36-1-1,64 | 0 | 0 | 0 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 30 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 2 | 0 | 0 | 0 | 2 |
0.80 | 5-36-1-1,80 | 10 | 20 | 70 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
5.12 | 5-36-1-4,62 | 0 | 0 | 0 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.62 | 5-36-1-5,62 | 50 | 45 | 5 | Pleistocene | VOLCANIC ASH | Minor lithology; relative abundance | 0 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
8.13 | 5-36-1-6,63 | 10 | 30 | 60 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 20 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
8.40 | 5-36-1-6,90 | 0 | 0 | 0 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
8.97 | 5-36-1-61,147 | 21 | 17 | 62 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 0 | 0 |
11.05 | 5-36-2-2,55 | 0 | 25 | 75 | Pleistocene | ZEOLITE BEARING CLAYEY MUD | Minor lithology; relative abundance | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
11.91 | 5-36-2-21,141 | 25 | 20 | 55 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 55 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
12.35 | 5-36-2-3,35 | 5 | 25 | 70 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
12.75 | 5-36-2-3,75 | 0 | 25 | 75 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
13.80 | 5-36-2-4,30 | 5 | 75 | 20 | Pleistocene | CLAYEY FORAM NANNO CHALK OOZE | Minor lithology; numerical abundance | 0 | 0 | 55 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
14.00 | 5-36-2-4,50 | 0 | 0 | 0 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
14.69 | 5-36-2-41,119 | 0 | 0 | 0 | Pleistocene | CARBONATE FORAM NANNO MARL MUD | Minor lithology; numerical abundance | 0 | 0 | 20 | 20 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
17.25 | 5-36-2-6,75 | 30 | 30 | 40 | Pleistocene | NANNO FORAM CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 40 | 60 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
18.20 | 5-36-3-1,20 | 20 | 20 | 60 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 60 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
18.71 | 5-36-3-1,71 | 0 | 25 | 75 | Pleistocene | CALCAREOUS CLAYEY MUD | Minor lithology; relative abundance | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
19.10 | 5-36-3-11,110 | 30 | 25 | 55 | Pleistocene | NANNO FORAM CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 40 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
21.08 | 5-36-3-3,8 | 0 | 25 | 75 | Pleistocene | CLAYEY FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
21.80 | 5-36-3-3,80 | 5 | 35 | 60 | Pleistocene | CALCAREOUS ZEOLITIC CLAY | Dominat lithology; numerical abundance | 10 | 0 | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
22.20 | 5-36-3-31,120 | 0 | 65 | 35 | Pleistocene | CALCAREOUS ZEOLITIC CLAY | Dominat lithology; numerical abundance | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
22.78 | 5-36-3-4,28 | 5 | 5 | 90 | Pleistocene | NANNO CHALK OOZE | Minor lithology; numerical abundance | 0 | 0 | 90 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
22.90 | 5-36-3-4,40 | 0 | 60 | 40 | Pleistocene | ZEOLITIC CLAY | Dominat lithology; relative abundance | 1 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
23.50 | 5-36-3-41,100 | 5 | 5 | 90 | Pleistocene | NANNO CHALK OOZE | Minor lithology; numerical abundance | 0 | 0 | 90 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
23.85 | 5-36-3-41,135 | 0 | 10 | 90 | Pleistocene | NANNO CLAYEY MUD | Minor lithology; relative abundance | 0 | 0 | 40 | 5 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
24.17 | 5-36-3-5,17 | 0 | 30 | 70 | Pleistocene | ZEOLITIC CLAYEY MUD | Dominat lithology; relative abundance | 2 | 0 | 2 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 25 | 65 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
24.80 | 5-36-3-5,80 | 0 | 40 | 60 | Pleistocene | NANNO BEARING ZEOLITIC CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 25 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
25.40 | 5-36-3-51,140 | 5 | 15 | 80 | Pleistocene | CLAYEY FORAM NANNO CHALK OOZE | Minor lithology; numerical abundance | 0 | 0 | 65 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
26.20 | 5-36-3-6,70 | 10 | 20 | 70 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
26.90 | 5-36-3-61,140 | 30 | 30 | 40 | Pleistocene | NANNO FORAM CHALK OOZE | Minor lithology; relative abundance | 0 | 0 | 30 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
27.80 | 5-36-4-1,80 | 10 | 10 | 80 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
27.88 | 5-36-4-1,88 | 15 | 20 | 65 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 25 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
28.40 | 5-36-4-11,140 | 10 | 10 | 80 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
29.30 | 5-36-4-2,80 | 0 | 0 | 0 | Pleistocene | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
29.60 | 5-36-4-21,110 | 0 | 30 | 70 | Pleistocene | NANNO FORAM CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 69 | 30 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
30.60 | 5-36-4-3,60 | 0 | 30 | 70 | Pleistocene | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
30.70 | 5-36-4-3,70 | 0 | 0 | 0 | Pleistocene | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
32.43 | 5-36-4-4,93 | 0 | 30 | 70 | Pleistocene | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 29 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 14 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
34.10 | 5-36-4-51,110 | 0 | 30 | 70 | Pleistocene | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
34.95 | 5-36-4-6,45 | 15 | 10 | 75 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 25 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
35.12 | 5-36-4-6,62 | 45 | 35 | 20 | Pleistocene | CALCAREOUS VOLCANIC ASH | Minor lithology; numerical abundance | 0 | 0 | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 70 | 0 | 0 | 0 | 0 |
35.60 | 5-36-4-61,110 | 15 | 15 | 70 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
39.94 | 5-36-5-3,94 | 0 | 30 | 70 | Pleistocene | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 65 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
40.80 | 5-36-5-4,30 | 5 | 95 | 0 | Pleistocene | NANNO CHALK OOZE | Minor lithology; relative abundance | 0 | 0 | 80 | 20 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
41.75 | 5-36-5-41,125 | 5 | 25 | 70 | Pleistocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
48.90 | 5-36-6-1,90 | 0 | 30 | 70 | Upper pliocene | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
50.00 | 5-36-6-2,50 | 0 | 30 | 70 | Upper pliocene | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
50.19 | 5-36-6-2,69 | 0 | 20 | 80 | Upper pliocene | CLAY WITH FORAMS AND GLASS | Minor lithology; relative abundance | 0 | 0 | 2 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
53.50 | 5-36-6-41,100 | 0 | 30 | 70 | Upper pliocene | NANNO FORAM CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
66.83 | 5-36-8-1,83 | 0 | 5 | 95 | Upper pliocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
69.25 | 5-36-8-3,25 | 0 | 20 | 80 | Lower pliocene | FORAM CLAY | Dominat lithology; numerical abundance | 0 | 0 | 5 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
69.80 | 5-36-8-3,80 | 0 | 15 | 85 | Lower pliocene | FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 85 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
70.45 | 5-36-8-31,145 | 0 | 30 | 70 | Lower pliocene | FORAM CLAY | Dominat lithology; relative abundance | 0 | 0 | 5 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
73.00 | 5-36-8-51,100 | 0 | 0 | 0 | Lower pliocene | NANNO BEARING CLAYEY MUD | Minor lithology; relative abundance | 2 | 0 | 10 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
74.20 | 5-36-8-6,70 | 0 | 30 | 70 | Lower pliocene | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
77.10 | 5-36-9-2,60 | 0 | 5 | 95 | Lower pliocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 94 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
78.60 | 5-36-9-3,60 | 0 | 5 | 95 | Lower pliocene | CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 2 | 1 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
83.25 | 5-36-10-1,25 | 0 | 2 | 98 | Lower pliocene | CLAYEY MUD | Minor lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
83.70 | 5-36-10-1,70 | 0 | 10 | 90 | Lower pliocene | CLAYEY COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 80 | 3 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
84.35 | 5-36-10-11,135 | 0 | 3 | 97 | Lower pliocene | COCCOLITH CHALK OOZE | Minor lithology; numerical abundance | 0 | 0 | 95 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
85.10 | 5-36-10-2,60 | 0 | 0 | 100 | Lower pliocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 90 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
85.43 | 5-36-10-2,93 | 10 | 60 | 30 | Lower pliocene | VOLCANIC GLASS | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 70 | 0 | 0 | 0 | 0 |
86.40 | 5-36-10-3,40 | 0 | 2 | 98 | Lower pliocene | CLAYEY MUD | Minor lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
87.20 | 5-36-10-31,120 | 0 | 2 | 98 | Lower pliocene | CLAYEY COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 88 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
91.60 | 5-36-10-61,110 | 0 | 3 | 97 | Lower pliocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 7 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
93.80 | 5-36-11-2,30 | 0 | 3 | 97 | Lower pliocene | CLAYEY MUD | Dominat lithology; numerical abundance | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 93 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
95.06 | 5-36-11-3,6 | 0 | 1 | 99 | Lower pliocene | CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
95.50 | 5-36-11-3,50 | 0 | 0 | 0 | Lower pliocene | NANNO CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 20 | 2 | 2 | 0 | 2 | 3 | 0 | 0 | 0 | 72 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
95.93 | 5-36-11-3,93 | 0 | 0 | 0 | Lower pliocene | CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 97 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
96.40 | 5-36-11-31,140 | 3 | 7 | 90 | Lower pliocene | CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 4 | 0 | 0 | 0 | 90 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
97.00 | 5-36-11-4,50 | 3 | 4 | 93 | Lower pliocene | NANNO CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 2 | 1 | 0 | 2 | 73 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
97.77 | 5-36-11-41,127 | 0 | 2 | 98 | Lower pliocene | CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 93 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
98.60 | 5-36-11-5,60 | 0 | 10 | 90 | Lower pliocene | CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 5 | 3 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 85 | 0 | 2 | 1 | 0 | 0 | 0 | 0 |
99.37 | 5-36-11-51,137 | 0 | 0 | 100 | Lower pliocene | NANNO CHALK OOZE | Minor lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
99.90 | 5-36-11-6,40 | 0 | 2 | 98 | Lower pliocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
100.70 | 5-36-11-61,120 | 0 | 2 | 98 | Lower pliocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
102.10 | 5-36-12-1,10 | 0 | 2 | 98 | Lower pliocene | NANNO CLAYEY MUD | Minor lithology; relative abundance | 0 | 0 | 30 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 68 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
102.70 | 5-36-12-1,70 | 4 | 5 | 91 | Lower pliocene | CLAYEY NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 71 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 4 | 0 | 0 | 0 | 0 |
103.40 | 5-36-12-11,140 | 0 | 0 | 0 | Lower pliocene | CLAYEY NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 75 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 4 | 0 | 0 | 0 | 0 |
104.10 | 5-36-12-2,60 | 0 | 2 | 98 | Upper miocene | CLAYEY MUD | Minor lithology; numerical abundance | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 90 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
104.30 | 5-36-12-2,80 | 0 | 0 | 100 | Upper miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 2 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
108.75 | 5-36-12-5,75 | 0 | 0 | 100 | Upper miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
109.50 | 5-36-12-51,150 | 0 | 0 | 0 | Upper miocene | VOLCANIC GLASS | Minor lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
109.78 | 5-36-12-6,28 | 0 | 0 | 100 | Upper miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
109.87 | 5-36-12-6,37 | 0 | 0 | 100 | Upper miocene | CLAYEY MUD WITH NANNOS | Minor lithology; relative abundance | 0 | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 85 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
110.42 | 5-36-12-6,92 | 0 | 0 | 100 | Lower miocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 95 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
110.54 | 5-36-12-61,104 | 0 | 0 | 100 | Lower miocene | CLAYEY MUD | Minor lithology; relative abundance | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
113.70 | 5-36-13-21,120 | 0 | 0 | 100 | Lower miocene | CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 100 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
114.50 | 5-36-13-3,50 | 0 | 0 | 100 | Lower miocene | CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
114.70 | 5-36-13-3,70 | 2 | 2 | 96 | Lower miocene | CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 3 | 2 | 4 | 2 | 2 | 0 | 0 | 0 | 0 | 93 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
116.20 | 5-36-13-4,70 | 8 | 10 | 82 | Lower miocene | SILICEOUS FOSSIL CLAYEY MUD | Dominat lithology; relative abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 77 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |