Ryan, William B F; Hsü, Kenneth J (2005): Smear slide analysis of Hole 13-132 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230366
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
Kaneps, Ansis G; Wezel, Forese C; Stradner, Herbert; Pautot, Guy; Nesteroff, Wladimir D; Maync, Wolf; Llort, Jennifer; Dumitrica, Paulian; Cita, Maria Bianca; Ryan, William B F; Hsü, Kenneth J (1973): Initial Reports of the Deep Sea Drilling Project 13. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIII, 514 pp, https://doi.org/10.2973/dsdp.proc.13.1973
Further details:
Project(s):
Funding:
Sixth Framework Programme (FP6), grant/award no. 36949: Southern European Seas: Assessing and Modelling Ecosystem Changes
Coverage:
Latitude: 40.261700 * Longitude: 11.441200
Date/Time Start: 1970-09-24T00:00:00 * Date/Time End: 1970-09-24T00:00:00
Minimum DEPTH, sediment/rock: 0.45 m * Maximum DEPTH, sediment/rock: 220.74 m
Event(s):
13-132 * Latitude: 40.261700 * Longitude: 11.441200 * Date/Time: 1970-09-24T00:00:00 * Elevation: -2835.0 m * Penetration: 223 m * Recovery: 165.3 m * Location: Mediterranean Sea/CONT RISE * Campaign: Leg13 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 26 cores; 214 m cored; 9 m drilled; 77.2 % 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 | 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 | Spiculae | Spiculae | % | Smear slide analysis | ||
15 | Anhydrite | Anh | % | Smear slide analysis | ||
16 | Gypsum | Gp | % | Smear slide analysis | ||
17 | Quartz | Qz | % | Smear slide analysis | ||
18 | Feldspar | Fsp | % | Smear slide analysis | ||
19 | Mica | Mica | % | Smear slide analysis | ||
20 | Clay minerals | Clay min | % | Smear slide analysis | ||
21 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
22 | Iron | Fe | % | Smear slide analysis | ||
23 | Limonite | Lm | % | Smear slide analysis | ||
24 | Epidote | Ep | % | Smear slide analysis | ||
25 | Hornblende | Hbl | % | Smear slide analysis | ||
26 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
27 | Rock fragments | Rock fragm | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3406 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 Spiculae [%] | 15 Anh [%] | 16 Gp [%] | 17 Qz [%] | 18 Fsp [%] | 19 Mica [%] | 20 Clay min [%] | 21 Py [%] | 22 Fe [%] | 23 Lm [%] | 24 Ep [%] | 25 Hbl [%] | 26 Volc glass [%] | 27 Rock fragm [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.45 | 13-132-1-1,20 | 0 | 30 | 70 | Upper pleistocene | MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 20 | 0 | 0 | 0 | 3 | 0 | 0 | 5 | 0 |
1.25 | 13-132-1-11,100 | 70 | 30 | 0 | Upper pleistocene | TEPHRA | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 5 | 70 | 0 |
1.45 | 13-132-1-11,120 | 20 | 20 | 60 | Upper pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 7 | 0 | 0 | 0 | 0 | 10 | 0 | 7 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 3 |
1.85 | 13-132-1-2,10 | 2 | 13 | 85 | Upper pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 80 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
2.88 | 13-132-1-21,113 | 10 | 20 | 70 | Upper pleistocene | MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 40 | 10 | 0 | 0 | 0 | 0 | 15 | 0 | 20 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 |
3.03 | 13-132-1-21,128 | 60 | 20 | 20 | Upper pleistocene | LITHIC SAND | Minor lithology; numerical abundance | 15 | 0 | 10 | 10 | 0 | 0 | 0 | 0 | 50 | 3 | 0 | 0 | 7 | 0 | 0 | 0 | 5 | 0 | 0 |
3.09 | 13-132-1-21,134 | 5 | 20 | 75 | Upper pleistocene | PYRITIC MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 40 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 10 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 |
3.35 | 13-132-1-3,10 | 80 | 20 | 0 | Upper pleistocene | TEPHRA | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 5 | 70 | 0 |
3.61 | 13-132-1-3,36 | 50 | 30 | 20 | Upper pleistocene | LITHIC SAND | Minor lithology; relative abundance | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 2 | 5 | 0 | 0 | 0 | 0 | 5 | 5 | 2 | 0 |
3.80 | 13-132-1-3,55 | 20 | 10 | 70 | Upper pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 15 | 0 | 0 | 0 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
3.91 | 13-132-1-3,66 | 20 | 10 | 70 | Upper pleistocene | MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 55 | 10 | 0 | 0 | 0 | 0 | 15 | 0 | 10 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 |
5.75 | 13-132-1-41,100 | 10 | 10 | 80 | Upper pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 77 | 7 | 0 | 0 | 0 | 0 | 7 | 0 | 5 | 0 | 1 | 0 | 3 | 0 | 0 | 0 | 0 |
7.17 | 13-132-1-5,92 | 10 | 10 | 80 | Upper pleistocene | PYRITIC MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 33 | 7 | 0 | 0 | 0 | 0 | 10 | 0 | 15 | 0 | 20 | 0 | 15 | 0 | 0 | 0 | 0 |
7.35 | 13-132-1-51,110 | 15 | 10 | 75 | Upper pleistocene | MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 56 | 15 | 0 | 0 | 0 | 0 | 7 | 0 | 10 | 0 | 7 | 2 | 3 | 0 | 0 | 0 | 0 |
8.25 | 13-132-1-6,50 | 20 | 10 | 70 | Upper pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 71 | 5 | 0 | 0 | 0 | 0 | 20 | 0 | 10 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 0 |
8.66 | 13-132-1-6,91 | 90 | 0 | 10 | Upper pleistocene | LITHIC SAND | Minor lithology; numerical abundance | 0 | 0 | 10 | 40 | 0 | 0 | 0 | 0 | 40 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 |
8.70 | 13-132-1-6,95 | 10 | 20 | 70 | Upper pleistocene | MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 58 | 15 | 0 | 2 | 0 | 0 | 7 | 0 | 7 | 0 | 3 | 3 | 0 | 0 | 0 | 5 | 0 |
8.71 | 13-132-1-6,96 | 40 | 30 | 30 | Upper pleistocene | FINE SAND-ARENITE | Minor lithology; numerical abundance | 10 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 10 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 |
8.98 | 13-132-1-61,123 | 60 | 30 | 10 | Upper pleistocene | TEPHRA | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 5 | 65 | 0 |
9.03 | 13-132-1-61,128 | 0 | 30 | 70 | Pleistocene | MARL OOZE WITH VOLCANIC GLASS | Minor lithology; numerical abundance | 0 | 0 | 55 | 3 | 0 | 0 | 0 | 0 | 10 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 25 | 0 |
9.20 | 13-132-1-61,145 | 50 | 30 | 20 | Pleistocene | LITHIC SAND | Dominat lithology; numerical abundance | 0 | 0 | 13 | 30 | 0 | 0 | 0 | 0 | 30 | 0 | 2 | 0 | 15 | 0 | 0 | 0 | 10 | 0 | 0 |
10.00 | 13-132-2-11,100 | 15 | 10 | 75 | Pleistocene | MARL OOZE WITH VOLCANIC GLASS | Dominat lithology; relative abundance | 0 | 0 | 52 | 7 | 2 | 1 | 0 | 0 | 10 | 0 | 5 | 0 | 3 | 0 | 2 | 0 | 0 | 20 | 0 |
10.07 | 13-132-2-11,107 | 0 | 40 | 60 | Pleistocene | PYRITIC CLAY WITH VOLCANIC GLASS | Minor lithology; numerical abundance | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 35 | 0 |
10.20 | 13-132-2-11,120 | 0 | 0 | 0 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
11.50 | 13-132-2-21,100 | 15 | 20 | 65 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 81 | 7 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 |
11.76 | 13-132-2-21,126 | 15 | 30 | 55 | Pleistocene | MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 52 | 7 | 0 | 0 | 0 | 0 | 20 | 0 | 15 | 0 | 0 | 3 | 0 | 0 | 0 | 3 | 0 |
13.25 | 13-132-2-31,125 | 0 | 20 | 80 | Pleistocene | PYRITIC CLAY WITH VOLCANIC GLASS | Minor lithology; numerical abundance | 0 | 0 | 18 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 0 | 50 | 0 | 2 | 0 | 0 | 23 | 0 |
14.50 | 13-132-2-41,100 | 10 | 5 | 85 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 86 | 5 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 |
14.54 | 13-132-2-41,104 | 15 | 5 | 80 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 79 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
14.57 | 13-132-2-41,107 | 5 | 15 | 80 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 83 | 5 | 0 | 0 | 0 | 0 | 7 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
19.00 | 13-132-3-11,100 | 3 | 10 | 87 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 83 | 3 | 0 | 0 | 0 | 0 | 5 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
19.14 | 13-132-3-11,114 | 15 | 15 | 70 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 76 | 10 | 0 | 0 | 0 | 0 | 7 | 0 | 3 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 |
20.30 | 13-132-3-2,80 | 20 | 20 | 60 | Pleistocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 50 | 15 | 0 | 0 | 0 | 0 | 15 | 0 | 10 | 0 | 3 | 0 | 1 | 0 | 0 | 2 | 4 |
21.70 | 13-132-3-3,70 | 15 | 0 | 85 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 84 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
23.51 | 13-132-3-41,101 | 0 | 30 | 70 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 74 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
28.40 | 13-132-4-11,140 | 10 | 20 | 70 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 10 | 0 | 0 | 0 | 0 | 7 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
29.50 | 13-132-4-21,100 | 0 | 10 | 90 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 84 | 2 | 0 | 0 | 0 | 0 | 7 | 0 | 4 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 |
29.67 | 13-132-4-21,117 | 0 | 20 | 80 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 77 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 7 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
31.98 | 13-132-4-4,48 | 60 | 20 | 20 | Pleistocene | VOLCANIC SAND | Minor lithology; numerical abundance | 0 | 0 | 10 | 3 | 0 | 0 | 0 | 0 | 10 | 2 | 15 | 0 | 10 | 0 | 0 | 0 | 0 | 50 | 0 |
33.60 | 13-132-4-5,60 | 90 | 0 | 10 | Pleistocene | LITHIC SAND (QUARTZOSE) | Minor lithology; numerical abundance | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 50 | 2 | 13 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 |
35.84 | 13-132-4-61,134 | 35 | 15 | 50 | Pleistocene | PYRITIC MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 30 | 30 | 0 | 0 | 0 | 0 | 10 | 0 | 5 | 0 | 20 | 5 | 0 | 0 | 0 | 0 | 0 |
38.40 | 13-132-5-2,90 | 0 | 10 | 90 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 82 | 3 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 |
46.25 | 13-132-6-11,125 | 0 | 15 | 85 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 87 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 |
49.85 | 13-132-6-4,35 | 85 | 10 | 5 | Lower pleistocene | FORAMINIFERAL SAND | Minor lithology; relative abundance | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 30 | 2 | 5 | 0 | 5 | 0 | 0 | 2 | 5 | 2 | 0 |
50.20 | 13-132-6-4,70 | 10 | 10 | 80 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 3 | 10 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
50.70 | 13-132-6-41,120 | 70 | 20 | 10 | Lower pleistocene | TEPHRA | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 65 | 0 |
51.80 | 13-132-6-5,80 | 5 | 5 | 90 | Lower pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 89 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 |
52.16 | 13-132-6-51,116 | 10 | 10 | 80 | Lower pleistocene | PYRITIC MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 60 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 |
52.17 | 13-132-6-51,117 | 10 | 5 | 85 | Lower pleistocene | PYRITIC MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 65 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 8 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 |
55.25 | 13-132-7-1,95 | 5 | 5 | 90 | Lower pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 82 | 10 | 0 | 0 | 0 | 0 | 3 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
58.47 | 13-132-7-31,117 | 5 | 5 | 90 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 85 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
62.90 | 13-132-7-61,110 | 5 | 5 | 90 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 83 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
65.66 | 13-132-8-21,116 | 5 | 10 | 85 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 85 | 5 | 0 | 0 | 0 | 0 | 3 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
66.18 | 13-132-8-3,18 | 15 | 15 | 70 | Lower pleistocene | PYRITIC MARL OOZE | Minor lithology; relative abundance | 0 | 0 | 35 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 10 | 30 | 15 | 0 | 0 | 2 | 0 | 0 | 0 |
68.60 | 13-132-8-41,110 | 2 | 13 | 85 | Lower pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 2 | 2 | 85 | 3 | 0 | 0 | 0 | 0 | 2 | 0 | 7 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
69.95 | 13-132-8-5,95 | 5 | 15 | 80 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 5 | 0 | 0 | 0 | 0 | 3 | 0 | 7 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 |
74.20 | 13-132-9-2,70 | 3 | 7 | 90 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 85 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
77.60 | 13-132-9-41,110 | 3 | 7 | 90 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 85 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
80.10 | 13-132-9-6,60 | 15 | 5 | 80 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 73 | 15 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
83.80 | 13-132-10-21,130 | 20 | 10 | 70 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 73 | 15 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 |
85.00 | 13-132-10-31,100 | 10 | 5 | 85 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 77 | 3 | 0 | 0 | 0 | 0 | 5 | 0 | 12 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 |
87.30 | 13-132-10-5,30 | 15 | 10 | 75 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 77 | 15 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 |
93.25 | 13-132-11-3,25 | 20 | 10 | 70 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 1 | 0 | 68 | 20 | 0 | 1 | 0 | 0 | 2 | 0 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
95.60 | 13-132-11-41,110 | 10 | 10 | 80 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 82 | 7 | 0 | 0 | 0 | 0 | 3 | 0 | 5 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 |
103.10 | 13-132-12-31,110 | 25 | 5 | 70 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 74 | 20 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 |
108.50 | 13-132-13-1,20 | 15 | 10 | 75 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 79 | 15 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
112.10 | 13-132-13-3,80 | 20 | 10 | 70 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 66 | 20 | 0 | 0 | 0 | 0 | 7 | 0 | 3 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 0 |
128.90 | 13-132-15-21,140 | 20 | 0 | 80 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 71 | 20 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
137.58 | 13-132-16-2,90 | 5 | 5 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 80 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 5 | 0 | 0 | 0 | 0 |
143.78 | 13-132-16-61,110 | 20 | 0 | 80 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 73 | 20 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
147.90 | 13-132-17-3,90 | 0 | 5 | 95 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 1 | 90 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
149.80 | 13-132-17-41,130 | 3 | 7 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 90 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
150.88 | 13-132-17-5,88 | 5 | 5 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 85 | 5 | 0 | 0 | 0 | 0 | 3 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
154.20 | 13-132-18-1,95 | 5 | 5 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 88 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
156.90 | 13-132-18-3,65 | 0 | 10 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 88 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
158.95 | 13-132-18-41,120 | 2 | 8 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 90 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
161.65 | 13-132-18-6,90 | 5 | 10 | 85 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 92 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
162.66 | 13-132-19-1,66 | 10 | 0 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 1 | 0 | 89 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
163.00 | 13-132-19-11,100 | 5 | 5 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 85 | 5 | 0 | 0 | 0 | 0 | 3 | 2 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
164.25 | 13-132-19-2,75 | 2 | 3 | 95 | Lower pliocene | NANNO ZONE | Dominat lithology; numerical abundance | 0 | 0 | 90 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
166.04 | 13-132-19-31,104 | 2 | 3 | 95 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 90 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
172.30 | 13-132-20-11,130 | 5 | 5 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 85 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
172.70 | 13-132-20-2,20 | 3 | 2 | 95 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 82 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 3 | 2 | 3 | 0 | 0 | 0 | 0 |
173.12 | 13-132-20-2,62 | 2 | 3 | 95 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 85 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
175.02 | 13-132-20-31,102 | 3 | 2 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 2 | 2 | 80 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
175.02 | 13-132-20-31,102 | 5 | 5 | 95 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 90 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
175.10 | 13-132-20-31,110 | 5 | 5 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 5 | 0 | 0 | 0 | 0 |
176.00 | 13-132-20-4,50 | 2 | 3 | 95 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
176.50 | 13-132-20-41,100 | 3 | 2 | 95 | Lower pliocene | NANNO OOZE (HEMATITIC) | Dominat lithology; relative abundance | 0 | 2 | 75 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
177.10 | 13-132-20-CC,0 | 10 | 5 | 85 | Lower pliocene | HEMATITIC MARL OOZE | Dominat lithology; numerical abundance | 4 | 0 | 60 | 10 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 |
177.10 | 13-132-20-CC,0 | 5 | 5 | 90 | Lower pliocene | NANNO OOZE | Minor lithology; numerical abundance | 0 | 0 | 80 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
180.70 | 13-132-21-1,70 | 0 | 0 | 0 | Lower pliocene | LIMONITIC MARL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 64 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 5 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 |
181.48 | 13-132-21-11,148 | 0 | 0 | 0 | Lower pliocene | LIMONITIC MARL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 3 | 0 | 20 | 0 | 0 | 0 | 0 |
182.05 | 13-132-21-2,55 | 5 | 5 | 90 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 2 | 80 | 5 | 0 | 0 | 0 | 0 | 3 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
182.07 | 13-132-21-2,57 | 0 | 0 | 0 | Lower pliocene | GOETHITE? | Minor lithology; numerical abundance | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 2 | 0 | 90 | 0 | 0 | 0 | 0 |
182.20 | 13-132-21-2,70 | 0 | 0 | 0 | Lower pliocene | HEMATITIC MARL OOZE | Minor lithology; numerical abundance | 0 | 0 | 52 | 2 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 |
182.26 | 13-132-21-2,76 | 5 | 10 | 85 | Upper miocene | HEMATITIC NANNO OOZE | Minor lithology; relative abundance | 0 | 2 | 77 | 5 | 0 | 0 | 0 | 0 | 3 | 0 | 5 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 |
182.32 | 13-132-21-2,82 | 5 | 15 | 80 | Upper miocene | ANHYDRITE AND GYPSUM | Minor lithology; numerical abundance | 0 | 3 | 10 | 2 | 0 | 0 | 45 | 10 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 |
182.38 | 13-132-21-2,88 | 0 | 0 | 0 | Upper miocene | ORGANIC SAND WITH GYPSUM | Minor lithology; numerical abundance | 20 | 0 | 0 | 40 | 0 | 0 | 0 | 35 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
182.45 | 13-132-21-2,95 | 0 | 0 | 0 | Upper miocene | ANHYDRITIC PYRITIC CLAY | Minor lithology; numerical abundance | 0 | 0 | 20 | 0 | 0 | 0 | 45 | 10 | 5 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 |
182.48 | 13-132-21-2,98 | 0 | 10 | 90 | Upper miocene | ANHYDRITE | Minor lithology; relative abundance | 0 | 2 | 15 | 0 | 0 | 0 | 60 | 5 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 |
182.52 | 13-132-21-21,102 | 5 | 15 | 80 | Upper miocene | ANHYDRITE-PYRITE MARL OOZE | Minor lithology; numerical abundance | 0 | 5 | 25 | 3 | 0 | 0 | 40 | 7 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 |
182.70 | 13-132-21-21,120 | 0 | 15 | 85 | Upper miocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 75 | 3 | 0 | 0 | 7 | 0 | 7 | 0 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
183.10 | 13-132-21-CC,0 | 5 | 20 | 70 | Upper miocene | HEMATITE MARL OOZE | Dominat lithology; numerical abundance | 0 | 2 | 55 | 7 | 0 | 0 | 20 | 0 | 3 | 0 | 15 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 5 |
183.10 | 13-132-21-CC,0 | 5 | 25 | 75 | Upper miocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 68 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 5 | 0 | 5 | 7 | 0 | 0 | 0 | 0 | 0 |
189.00 | 13-132-22-1,0 | 10 | 10 | 40 | Upper miocene | ANHYDRITE | Minor lithology; numerical abundance | 0 | 0 | 10 | 2 | 0 | 0 | 5 | 15 | 10 | 0 | 4 | 0 | 20 | 50 | 20 | 0 | 2 | 0 | 0 |
189.00 | 13-132-22-1,0 | 30 | 20 | 50 | Upper miocene | HEMATITE CLAY (RESIDUAL CLAY?) | Minor lithology; relative abundance | 0 | 0 | 0 | 2 | 0 | 0 | 75 | 2 | 0 | 0 | 0 | 0 | 0 | 50 | 20 | 0 | 0 | 0 | 0 |
189.00 | 13-132-22-1,0 | 5 | 50 | 85 | Upper miocene | RED OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
189.61 | 13-132-22-1,61 | 0 | 15 | 85 | Upper miocene | MARL OOZE WITH ANHYDRITE | Minor lithology; numerical abundance | 0 | 0 | 67 | 0 | 0 | 0 | 15 | 0 | 3 | 0 | 10 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 |
189.88 | 13-132-22-1,88 | 0 | 0 | 0 | Upper miocene | GYPSUM | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 |
190.10 | 13-132-22-11,110 | 0 | 30 | 70 | Upper miocene | ANHYDRITE MARL OOZE | Dominat lithology; relative abundance | 0 | 2 | 65 | 0 | 0 | 0 | 25 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
190.25 | 13-132-22-11,125 | 0 | 0 | 0 | Upper miocene | HEMATITE AND GYPSUM | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
190.30 | 13-132-22-11,130 | 0 | 0 | 0 | Upper miocene | GYPSUM | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
190.35 | 13-132-22-11,135 | 0 | 0 | 0 | Upper miocene | GYPSUM | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
190.45 | 13-132-22-11,145 | 25 | 45 | 30 | Upper miocene | GYPSUM AND ANHYDRITE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 55 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
191.00 | 13-132-23-1,0 | 0 | 0 | 0 | Upper miocene | GYPSUM | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
191.95 | 13-132-23-1,95 | 0 | 0 | 0 | Upper miocene | GYPSUM | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
192.10 | 13-132-23-11,110 | 2 | 13 | 85 | Upper miocene | ANHYDRITE | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 95 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
207.46 | 13-132-25-1,46 | 0 | 10 | 90 | Upper miocene | ANHYDRITE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 92 | 3 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
207.91 | 13-132-25-1,91 | 0 | 10 | 90 | Upper miocene | ANHYDRITE LIMONITE STAINED | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 30 | 0 | 0 | 0 | 0 |
208.60 | 13-132-25-2,10 | 10 | 20 | 70 | Upper miocene | GYPSIPHEROUS ANHYDRITE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 10 | 0 | 0 | 0 | 0 | 5 | 3 | 7 | 0 | 0 | 2 | 0 |
209.35 | 13-132-25-2,85 | 20 | 10 | 70 | Upper miocene | HEMATITE ANHYDRITE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 15 | 0 | 0 | 0 | 0 | 5 | 30 | 0 | 0 | 0 | 0 | 0 |
209.68 | 13-132-25-21,118 | 40 | 50 | 10 | Upper miocene | PYRITIZED SELENITIC SILT | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 |
209.75 | 13-132-25-21,125 | 3 | 12 | 85 | Upper miocene | ANHYDRITE | Dominat lithology; numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 80 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
214.00 | 13-132-26-1,0 | 5 | 35 | 60 | Upper miocene | ANHYDRITE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 10 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 |
214.59 | 13-132-26-1,59 | 10 | 20 | 70 | Upper miocene | ANHYDRITE | Dominat lithology; numerical abundance | 0 | 5 | 5 | 0 | 0 | 0 | 75 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
214.93 | 13-132-26-1,93 | 0 | 30 | 70 | Upper miocene | ANHYDRITE | Dominat lithology; numerical abundance | 0 | 3 | 20 | 0 | 0 | 0 | 65 | 7 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
215.13 | 13-132-26-11,113 | 5 | 15 | 80 | Upper miocene | HEMATITIC ANHYDRITE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 5 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 |
220.00 | 13-132-27-1,0 | 0 | 0 | 0 | Upper miocene | GYPSUM | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
220.69 | 13-132-27-1,69 | 0 | 0 | 0 | Upper miocene | GYPSUM | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
220.74 | 13-132-27-1,74 | 0 | 0 | 0 | Upper miocene | GYPSUM | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |