Lewis, Brian T R; Robinson, Paul T (2005): Smear slide analysis of Hole 65-483. PANGAEA, https://doi.org/10.1594/PANGAEA.230929
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
Zolotarev, Boris P; Stephen, Ralph A; Schmincke, Hans-Ulrich; Salisbury, Matthew H; Rangin, Claude; Morrison, M Ann; Kudo, A M; Hattner, J; Gutiérrez-Estrada, Mario; Flower, Martin F J; Duennebier, Frederick K; Day, Ron; Cambon, P; Blackinton, Grant; Benson, Richard N; Lewis, Brian T R; Robinson, P (1983): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXV, 752 pp, https://doi.org/10.2973/dsdp.proc.65.1983
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 22.883300 * Longitude: -108.748300
Date/Time Start: 1979-02-12T00:00:00 * Date/Time End: 1979-02-12T00:00:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 200.45 m
Event(s):
65-483 * Latitude: 22.883300 * Longitude: -108.748300 * Date/Time: 1979-02-12T00:00:00 * Elevation: -3070.0 m * Penetration: 204.5 m * Recovery: 110.7 m * Location: North Pacific/Gulf of California/CONT RISE * Campaign: Leg65 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 26 cores; 204.5 m cored; 0 m drilled; 54.1 % 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 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Quartz | Qz | % | Smear slide analysis | ||
18 | Feldspar | Fsp | % | Smear slide analysis | ||
19 | Zeolite | Zeo | % | Smear slide analysis | ||
20 | Mica | Mica | % | Smear slide analysis | ||
21 | Clay minerals | Clay min | % | Smear slide analysis | ||
22 | Glauconite | Glt | % | Smear slide analysis | ||
23 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
24 | Heavy minerals | HM | % | Smear slide analysis | ||
25 | Epidote | Ep | % | Smear slide analysis | ||
26 | Amphibole | Amp | % | Smear slide analysis | ||
27 | Sphene | Spn | % | Smear slide analysis | ||
28 | Pyroxene | Pyrox | % | Smear slide analysis | ||
29 | Volcanic glass | Volc glass | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1958 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 Silicoflag [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Mica [%] | 21 Clay min [%] | 22 Glt [%] | 23 Py [%] | 24 HM [%] | 25 Ep [%] | 26 Amp [%] | 27 Spn [%] | 28 Pyrox [%] | 29 Volc glass [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.02 | 65-483-1-1,2 | 0 | 37 | 63 | Upper quaternary | SILTY CLAY- CALC NANNO OOZE | Dominat lithology; relative abundance | 1 | 0 | 35 | 1 | 1 | 0 | 2 | 1 | 5 | 0 | 0 | 0 | 63 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 |
0.12 | 65-483-1-1,12 | 0 | 12 | 78 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 2 | 0 | 1 | 1 | 0 | 2 | 2 | 2 | 8 | 1 | 0 | 0 | 78 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 |
0.28 | 65-483-1-1,28 | 3 | 57 | 40 | Upper quaternary | CALC NANNO CLAYEY SILT | Dominat lithology; relative abundance | 5 | 0 | 35 | 0 | 2 | 3 | 0 | 3 | 10 | 0 | 0 | 2 | 40 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 |
1.07 | 65-483-2-1,7 | 5 | 40 | 55 | Upper quaternary | CALC NANNO SILTY CLAY | Dominat lithology; numerical abundance | 1 | 0 | 25 | 1 | 2 | 5 | 0 | 0 | 10 | 2 | 0 | 0 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
2.40 | 65-483-2-11,140 | 0 | 60 | 40 | Upper quaternary | DIATOMACEOUS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 2 | 0 | 15 | 40 | 1 | 1 | 1 | 0 | 0 | 0 | 40 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
3.00 | 65-483-2-2,50 | 0 | 63 | 37 | Upper quaternary | RADIOLARIAN DIATOMACEOUS OOZE | Dominat lithology; relative abundance | 0 | 0 | 1 | 0 | 20 | 30 | 1 | 5 | 5 | 0 | 0 | 2 | 37 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
4.12 | 65-483-2-3,12 | 0 | 70 | 30 | Upper quaternary | RADIOLARIAN DIATOMACEOUS OOZE | Dominat lithology; relative abundance | 1 | 0 | 4 | 0 | 15 | 35 | 0 | 5 | 8 | 1 | 0 | 0 | 30 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 |
4.53 | 65-483-2-3,53 | 3 | 70 | 27 | Upper quaternary | DIATOMACEOUS OOZE | Dominat lithology; relative abundance | 1 | 0 | 3 | 0 | 10 | 50 | 5 | 2 | 3 | 2 | 0 | 2 | 27 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
4.62 | 65-483-2-3,62 | 0 | 40 | 60 | Upper quaternary | CALC NANNO OOZE (GRAYISH OLIVE) | Dominat lithology; relative abundance | 0 | 0 | 25 | 0 | 10 | 5 | 0 | 0 | 3 | 2 | 0 | 0 | 60 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
5.41 | 65-483-2-31,141 | 0 | 62 | 48 | Upper quaternary | DIATOMACEOUS OOZE (OLIVE GRAY) | Dominat lithology; relative abundance | 1 | 0 | 5 | 0 | 20 | 30 | 2 | 5 | 2 | 0 | 0 | 2 | 48 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
10.55 | 65-483-3-1,5 | 3 | 52 | 45 | Upper quaternary | DIATOMACEOUS OOZE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 15 | 36 | 3 | 4 | 3 | 0 | 0 | 2 | 41 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
11.70 | 65-483-3-11,120 | 0 | 58 | 42 | Upper quaternary | DIATOMACEOUS CLAY | Dominat lithology; numerical abundance | 0 | 0 | 15 | 0 | 15 | 25 | 0 | 0 | 1 | 0 | 0 | 0 | 42 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
12.05 | 65-483-3-2,5 | 0 | 53 | 47 | Upper quaternary | Dominat lithology; numerical abundance | 0 | 0 | 0 | 1 | 5 | 16 | 2 | 7 | 10 | 5 | 0 | 1 | 47 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | |
12.99 | 65-483-3-2,99 | 0 | 58 | 42 | Upper quaternary | DIATOMACEOUS OOZE | relative abundance | 0 | 0 | 2 | 0 | 6 | 15 | 2 | 5 | 12 | 8 | 0 | 2 | 42 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 2 |
13.13 | 65-483-3-21,113 | 0 | 50 | 50 | Upper quaternary | DIATOMACEOUS OOZE | numerical abundance | 0 | 0 | 2 | 2 | 3 | 15 | 2 | 7 | 10 | 5 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
13.30 | 65-483-3-21,130 | 0 | 51 | 49 | Upper quaternary | DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 2 | 0 | 8 | 0 | 10 | 30 | 2 | 2 | 1 | 1 | 0 | 2 | 49 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
13.82 | 65-483-3-3,32 | 0 | 59 | 41 | Upper quaternary | DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 1 | 0 | 6 | 0 | 10 | 35 | 0 | 0 | 5 | 1 | 0 | 1 | 41 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 |
14.60 | 65-483-3-31,110 | 1 | 65 | 44 | Upper quaternary | DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 5 | 0 | 13 | 2 | 5 | 31 | 1 | 0 | 6 | 1 | 0 | 0 | 39 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
15.06 | 65-483-3-4,6 | 50 | 26 | 24 | Upper quaternary | SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 1 | 1 | 2 | 0 | 0 | 0 | 70 | 1 | 0 | 4 | 24 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
15.73 | 65-483-3-4,73 | 50 | 25 | 25 | Upper quaternary | SILTY SAND (ARKOSE) | Dominat lithology; relative abundance | 0 | 0 | 2 | 2 | 2 | 2 | 2 | 0 | 70 | 3 | 0 | 0 | 25 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 |
16.40 | 65-483-3-41,140 | 0 | 45 | 55 | Upper quaternary | DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 1 | 0 | 7 | 2 | 10 | 25 | 2 | 3 | 3 | 2 | 0 | 2 | 55 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
23.13 | 65-483-4-3,13 | 0 | 74 | 26 | Upper quaternary | DIATOMACEOUS CALC NANNO CLAY | Dominat lithology; relative abundance | 1 | 0 | 50 | 2 | 5 | 15 | 0 | 2 | 1 | 0 | 0 | 0 | 26 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
23.29 | 65-483-4-3,29 | 2 | 74 | 26 | Upper quaternary | DIATOMACEOUS CALC NANNO CLAY | Dominat lithology; numerical abundance | 1 | 0 | 50 | 1 | 5 | 15 | 1 | 1 | 2 | 0 | 0 | 0 | 26 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
24.22 | 65-483-4-31,122 | 10 | 74 | 16 | Upper quaternary | DIATOMACEOUS CALC NANNO CLAY | Minor lithology; relative abundance | 5 | 0 | 30 | 2 | 10 | 30 | 1 | 0 | 7 | 1 | 0 | 2 | 16 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
30.40 | 65-483-5-1,90 | 0 | 72 | 28 | Upper quaternary | RADS CALC NANNO DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 2 | 0 | 15 | 0 | 15 | 30 | 0 | 5 | 5 | 2 | 0 | 2 | 28 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
33.27 | 65-483-5-3,77 | 0 | 68 | 32 | Upper quaternary | DIATOMACEOUS CALC NANNOS CLAY | relative abundance | 3 | 0 | 30 | 2 | 5 | 20 | 0 | 0 | 5 | 1 | 0 | 2 | 32 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
33.37 | 65-483-5-3,87 | 0 | 44 | 56 | Upper quaternary | CALCAREOUS CLAY | Minor lithology; relative abundance | 4 | 0 | 30 | 2 | 0 | 0 | 0 | 5 | 1 | 2 | 0 | 0 | 56 | 0 | 4 | 2 | 0 | 0 | 0 | 0 | 0 |
36.61 | 65-483-5-51,111 | 0 | 54 | 46 | Upper quaternary | SILTY CLAY | relative abundance | 2 | 0 | 3 | 2 | 15 | 10 | 2 | 5 | 15 | 2 | 0 | 2 | 46 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 |
39.75 | 65-483-6-1,75 | 0 | 75 | 25 | Upper quaternary | CALCAREOUS NANNO CLAY | Dominat lithology; relative abundance | 3 | 0 | 35 | 2 | 10 | 20 | 0 | 0 | 5 | 2 | 0 | 2 | 25 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
40.78 | 65-483-6-2,28 | 5 | 67 | 28 | Upper quaternary | DIATOMACEOUS RADIOLARIAN CLAY | Dominat lithology; relative abundance | 1 | 0 | 1 | 0 | 20 | 20 | 0 | 30 | 2 | 2 | 0 | 2 | 28 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
40.80 | 65-483-6-2,30 | 70 | 20 | 10 | Upper quaternary | ASH FALL | Dominat lithology; relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 86 |
40.87 | 65-483-6-2,37 | 20 | 60 | 20 | Upper quaternary | SILTY CLAY WITH GLASS SHARDS | Dominat lithology; relative abundance | 1 | 0 | 15 | 2 | 15 | 15 | 0 | 2 | 1 | 2 | 0 | 0 | 20 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 30 |
41.25 | 65-483-6-2,75 | 0 | 42 | 58 | Upper quaternary | DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 1 | 0 | 15 | 20 | 0 | 5 | 1 | 2 | 0 | 2 | 58 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 |
42.42 | 65-483-6-3,42 | 20 | 55 | 25 | Upper quaternary | SILTY CLAY WITH FRACTION OF GLASS SHARDM QTZ 5,FEL TR,CLAY 25,VOLC.GLAS | Dominat lithology; numerical abundance | 0 | 0 | 5 | 0 | 10 | 15 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
42.75 | 65-483-6-3,75 | 0 | 38 | 62 | Upper quaternary | SULFIDE ENRICHED SILTY CLAY | Minor lithology; relative abundance | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 10 | 3 | 0 | 0 | 62 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 |
42.86 | 65-483-6-3,86 | 30 | 30 | 40 | Upper quaternary | SILTY SAND | Dominat lithology; relative abundance | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 50 | 5 | 0 | 0 | 40 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
49.24 | 65-483-7-1,74 | 5 | 40 | 55 | Upper quaternary | SILTY CLAY WITH TRACES OF ASH FALL | Dominat lithology; relative abundance | 0 | 0 | 0 | 2 | 10 | 15 | 0 | 10 | 5 | 2 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
49.79 | 65-483-7-11,129 | 0 | 4 | 96 | Upper quaternary | CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 3 | 2 | 0 | 0 | 96 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
50.15 | 65-483-7-2,15 | 0 | 50 | 50 | Upper quaternary | CLAYSTONE W/SAND SIZED PCES OF BLK GLASM QTZ 20,FEL 15,MICA 5,HVY.MINS 5 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
50.16 | 65-483-7-2,16 | 0 | 1 | 99 | Upper quaternary | CLAY WITH SHARDS OF GLASS | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
50.22 | 65-483-7-2,22 | 0 | 17 | 83 | Upper quaternary | CLAY | relative abundance | 0 | 0 | 5 | 2 | 5 | 5 | 2 | 2 | 2 | 0 | 0 | 0 | 83 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
50.75 | 65-483-7-2,75 | 0 | 55 | 45 | Upper quaternary | SILTY CLAY-DIATOMACEOUS SILTY CLAY | Dominat lithology; numerical abundance | 2 | 0 | 3 | 0 | 13 | 17 | 0 | 9 | 9 | 5 | 0 | 0 | 39 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
52.25 | 65-483-7-3,75 | 0 | 18 | 82 | Upper quaternary | CLAY WITH GLASS SHARD | relative abundance | 0 | 0 | 2 | 0 | 1 | 5 | 0 | 5 | 2 | 2 | 0 | 0 | 82 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 |
53.75 | 65-483-7-4,75 | 0 | 15 | 85 | Upper quaternary | CLAY | relative abundance | 2 | 0 | 5 | 2 | 2 | 5 | 0 | 0 | 2 | 2 | 0 | 0 | 85 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 |
54.75 | 65-483-7-5,25 | 0 | 50 | 50 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 3 | 0 | 3 | 3 | 0 | 5 | 0 | 0 | 15 | 6 | 0 | 5 | 50 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 |
55.06 | 65-483-7-5,56 | 0 | 15 | 85 | Upper quaternary | CLAYEY VOLCANIC ASH FALL | Minor lithology; relative abundance | 0 | 0 | 5 | 0 | 1 | 2 | 0 | 5 | 3 | 0 | 0 | 4 | 85 | 2 | 1 | 0 | 2 | 2 | 2 | 0 | 10 |
58.69 | 65-483-8-1,69 | 0 | 58 | 42 | Quaternary | CLAY | numerical abundance | 3 | 3 | 5 | 3 | 0 | 3 | 0 | 0 | 20 | 15 | 0 | 3 | 42 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 1 |
59.12 | 65-483-8-11,112 | 0 | 65 | 35 | Quaternary | SILTY CLAY (OOZE OF COCCOLITHS) | numerical abundance | 5 | 5 | 15 | 3 | 0 | 2 | 0 | 0 | 20 | 10 | 0 | 5 | 35 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
59.64 | 65-483-8-2,14 | 0 | 50 | 50 | Quaternary | SILTY CLAY | numerical abundance | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 4 | 25 | 14 | 0 | 0 | 50 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 |
61.61 | 65-483-8-3,61 | 0 | 50 | 50 | Quaternary | CLAY | relative abundance | 0 | 0 | 0 | 2 | 2 | 3 | 0 | 2 | 20 | 10 | 0 | 15 | 50 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 |
61.92 | 65-483-8-3,92 | 50 | 20 | 30 | Quaternary | SILTY SAND | relative abundance | 4 | 0 | 0 | 1 | 1 | 3 | 2 | 0 | 30 | 20 | 0 | 5 | 30 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 |
67.90 | 65-483-9-1,40 | 0 | 70 | 30 | Lower quaternary | PELAGIC CLAYEY SILT | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 9 | 3 | 0 | 0 | 37 | 0 | 49 | 0 | 0 | 0 | 0 | 0 | 0 |
68.25 | 65-483-9-1,75 | 5 | 55 | 40 | Lower quaternary | DIATOMACEOUS MUD | Dominat lithology; numerical abundance | 0 | 0 | 4 | 1 | 6 | 10 | 0 | 1 | 12 | 10 | 0 | 10 | 40 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 |
71.25 | 65-483-9-3,75 | 0 | 50 | 50 | Lower quaternary | CLAY (DIATOMACEOUS MUD) | Dominat lithology; numerical abundance | 0 | 0 | 2 | 1 | 0 | 8 | 0 | 0 | 15 | 8 | 0 | 15 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
72.75 | 65-483-9-4,75 | 5 | 60 | 35 | Lower quaternary | DIATOMACEOUS MUD | numerical abundance | 0 | 0 | 12 | 0 | 6 | 18 | 0 | 0 | 12 | 6 | 0 | 0 | 41 | 0 | 2 | 4 | 0 | 0 | 0 | 0 | 0 |
86.77 | 65-483-11-1,27 | 0 | 43 | 57 | Lower quaternary | MUD (CLAYSTONE) | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 20 | 10 | 0 | 2 | 57 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 5 |
87.25 | 65-483-11-1,75 | 1 | 10 | 89 | Lower quaternary | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 2 | 0 | 0 | 89 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 |
93.04 | 65-483-11-5,54 | 0 | 30 | 70 | Lower quaternary | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 7 | 0 | 0 | 70 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 |
106.50 | 65-483-13-11,100 | 0 | 30 | 70 | Lower quaternary | PELAGIC BIOGENIC | Dominat lithology; numerical abundance | 0 | 0 | 10 | 0 | 1 | 0 | 0 | 0 | 7 | 2 | 0 | 2 | 70 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
109.30 | 65-483-13-3,80 | 2 | 30 | 68 | Lower quaternary | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 10 | 2 | 1 | 68 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 1 |
142.05 | 65-483-17-1,5 | 3 | 60 | 37 | Upper pliocene | SILTSTONE | Minor lithology; numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 10 | 10 | 5 | 37 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 15 |
152.23 | 65-483-18-11,123 | 2 | 46 | 52 | Upper pliocene | SILTSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 10 | 10 | 2 | 52 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 1 |
152.86 | 65-483-18-2,36 | 5 | 40 | 55 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 0 | 1 | 15 | 5 | 1 | 55 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 15 |
153.76 | 65-483-18-21,126 | 30 | 46 | 24 | Upper pliocene | SANDY SILT | Dominat lithology; relative abundance | 2 | 0 | 1 | 2 | 0 | 0 | 2 | 0 | 30 | 15 | 3 | 3 | 24 | 0 | 5 | 1 | 0 | 0 | 0 | 10 | 10 |
155.00 | 65-483-18-31,100 | 30 | 34 | 38 | Upper pliocene | SANDY SILT | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 35 | 12 | 2 | 2 | 38 | 0 | 10 | 2 | 0 | 0 | 0 | 5 | 1 |
155.24 | 65-483-18-31,124 | 25 | 30 | 45 | Upper pliocene | SILTY CLAY (DIATOMACEOUS MUD) | numerical abundance | 0 | 0 | 3 | 0 | 0 | 2 | 2 | 0 | 20 | 10 | 0 | 5 | 45 | 0 | 8 | 4 | 0 | 0 | 0 | 0 | 1 |
155.87 | 65-483-18-4,37 | 5 | 45 | 50 | Upper pliocene | SILTY CLAY | Minor lithology; relative abundance | 2 | 0 | 2 | 0 | 0 | 10 | 0 | 0 | 15 | 10 | 2 | 0 | 50 | 0 | 5 | 3 | 0 | 0 | 0 | 0 | 5 |
156.45 | 65-483-18-4,95 | 3 | 36 | 61 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 15 | 5 | 10 | 2 | 61 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 5 |
156.75 | 65-483-18-41,125 | 5 | 45 | 50 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 1 | 2 | 0 | 2 | 0 | 0 | 20 | 10 | 5 | 1 | 45 | 0 | 10 | 3 | 0 | 0 | 0 | 0 | 1 |
200.45 | 65-483-26-1,45 | 15 | 30 | 55 | SILTY CLAY - INDURATED SILTY CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 15 | 1 | 2 | 55 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 10 |