Benson, William E; Sheridan, Robert E (2005): Smear slide analysis of Hole 44-390A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230727
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Benson, William E; Enos, Paul; Freeman, Tom; Gradstein, Felix M; Murdmaa, Ivar O; Pastouret, L; Schmidt, Ronald R; Sheridan, Robert E; Stuermer, D H; Weaver, Fred M; Worstell, Paula J (1978): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XLIV, 1005 pp, https://doi.org/10.2973/dsdp.proc.44.1978
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 30.142300 * Longitude: -76.112300
Date/Time Start: 1975-08-29T00:00:00 * Date/Time End: 1975-08-29T00:00:00
Minimum DEPTH, sediment/rock: 10.52 m * Maximum DEPTH, sediment/rock: 140.60 m
Event(s):
44-390A * Latitude: 30.142300 * Longitude: -76.112300 * Date/Time: 1975-08-29T00:00:00 * Elevation: -2665.0 m * Penetration: 142.5 m * Recovery: 86.3 m * Location: North Atlantic Ocean * Campaign: Leg44 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 14 cores; 133 m cored; 0 m drilled; 64.9 % 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 | Chalcedony | Chalcedony | % | Smear slide analysis | ||
14 | Chert | Chert | % | Smear slide analysis | fragments | |
15 | Radiolarians | Rad | % | Smear slide analysis | ||
16 | Diatoms | Diatoms | % | Smear slide analysis | ||
17 | Spiculae | Spiculae | % | Smear slide analysis | ||
18 | Minerals, other | Min other | % | Smear slide analysis | ||
19 | Quartz | Qz | % | Smear slide analysis | ||
20 | Feldspar | Fsp | % | Smear slide analysis | ||
21 | Zeolite | Zeo | % | Smear slide analysis | ||
22 | Mica | Mica | % | Smear slide analysis | ||
23 | Clay minerals | Clay min | % | Smear slide analysis | ||
24 | Opaque minerals | Opaque | % | Smear slide analysis | ||
25 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
26 | Iron | Fe | % | Smear slide analysis | ||
27 | Heavy minerals | HM | % | Smear slide analysis | ||
28 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
29 | Manganese | Mn | % | Smear slide analysis | ||
30 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2492 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 Chalcedony [%] | 14 Chert [%] | 15 Rad [%] | 16 Diatoms [%] | 17 Spiculae [%] | 18 Min other [%] | 19 Qz [%] | 20 Fsp [%] | 21 Zeo [%] | 22 Mica [%] | 23 Clay min [%] | 24 Opaque [%] | 25 Py [%] | 26 Fe [%] | 27 HM [%] | 28 Volc glass [%] | 29 Mn [%] | 30 Terr [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
10.52 | 44-390A-1-11,102 | 0 | 60 | 40 | Middle eocene | NANNOFOSSIL OOZE | Dominat lithology; numerical abundance | 55 | 0 | 30 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
10.97 | 44-390A-1-11,147 | 0 | 0 | 0 | Middle eocene | ZEOLITES | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 88 | 2 | 10 | 0 | 0 | 2 | 2 | 0 | 0 | 0 |
11.10 | 44-390A-1-CC,0 | 0 | 50 | 50 | Middle eocene | CALCAREOUS OOZE | Dominat lithology; relative abundance | 75 | 0 | 19 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
20.10 | 44-390A-2-11,110 | 2 | 68 | 30 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 5 | 0 | 0 | 2 | 2 | 6 | 0 | 2 | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
21.60 | 44-390A-2-21,110 | 5 | 65 | 30 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 67 | 3 | 0 | 0 | 8 | 2 | 10 | 0 | 2 | 0 | 2 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
21.67 | 44-390A-2-21,117 | 5 | 75 | 20 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 1 | 0 | 0 | 10 | 4 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
22.10 | 44-390A-2-CC,0 | 5 | 55 | 40 | Middle eocene | SILICEOUS+ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 60 | 5 | 0 | 0 | 5 | 2 | 8 | 0 | 0 | 0 | 15 | 2 | 4 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
29.90 | 44-390A-3-11,140 | 5 | 65 | 30 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 67 | 8 | 0 | 0 | 8 | 2 | 10 | 0 | 2 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
30.75 | 44-390A-3-2,75 | 5 | 65 | 30 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 50 | 3 | 0 | 0 | 5 | 2 | 10 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
34.10 | 44-390A-3-41,110 | 1 | 70 | 20 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 50 | 5 | 0 | 0 | 5 | 2 | 10 | 0 | 1 | 0 | 8 | 1 | 5 | 0 | 0 | 0 | 2 | 2 | 0 | 0 |
34.10 | 44-390A-3-41,110 | 10 | 80 | 20 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 13 | 0 | 63 | 8 | 0 | 0 | 8 | 8 | 8 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
34.60 | 44-390A-3-CC,0 | 5 | 65 | 30 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 70 | 5 | 0 | 0 | 5 | 2 | 7 | 0 | 2 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
39.15 | 44-390A-4-1,75 | 0 | 0 | 0 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 40 | 1 | 0 | 0 | 15 | 5 | 20 | 0 | 0 | 0 | 0 | 0 | 9 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
40.70 | 44-390A-4-2,80 | 3 | 76 | 24 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 55 | 10 | 0 | 0 | 10 | 5 | 10 | 0 | 1 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
42.40 | 44-390A-4-31,100 | 1 | 70 | 30 | Middle eocene | SILICEOUS NANNOFOSSIL OOZE | Dominat lithology; relative abundance | 30 | 0 | 30 | 10 | 0 | 0 | 5 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 10 |
43.90 | 44-390A-4-41,100 | 5 | 65 | 30 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; numerical abundance | 20 | 0 | 45 | 5 | 0 | 0 | 10 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
45.40 | 44-390A-4-51,100 | 0 | 70 | 30 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 17 | 0 | 70 | 2 | 0 | 0 | 3 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
46.80 | 44-390A-4-6,90 | 5 | 75 | 20 | SILICEOUS NANNO OOZE | Dominat lithology; numerical abundance | 10 | 0 | 48 | 10 | 0 | 0 | 5 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
46.94 | 44-390A-4-61,104 | 0 | 40 | 60 | NANNO-BEARING LIMESTONE | Minor lithology; numerical abundance | 60 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
47.50 | 44-390A-4-CC,0 | 0 | 60 | 40 | Lower eocene | FORAMINIFERAL NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 75 | 7 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 10 | 1 | 3 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
48.35 | 44-390A-5-1,85 | 0 | 60 | 40 | Lower eocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 42 | 6 | 0 | 0 | 0 | 1 | 0 | 7 | 2 | 0 | 5 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
48.90 | 44-390A-5-11,140 | 15 | 5 | 80 | Lower eocene | FORAMINIFERAL NANNO OOZE | Dominat lithology; numerical abundance | 10 | 0 | 70 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
49.51 | 44-390A-5-2,51 | 5 | 55 | 40 | Lower eocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 35 | 0 | 20 | 10 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
49.54 | 44-390A-5-2,54 | 1 | 70 | 30 | Lower eocene | NANNO CHALK | Minor lithology; numerical abundance | 30 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
49.58 | 44-390A-5-2,58 | 0 | 40 | 60 | Lower eocene | LIMESTONE | Minor lithology; relative abundance | 45 | 0 | 20 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
50.03 | 44-390A-5-21,103 | 0 | 40 | 60 | Lower eocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 13 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 0 | 5 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
51.02 | 44-390A-5-3,52 | 5 | 55 | 40 | Lower eocene | SILICEOUS NANNO OOZE | Dominat lithology; numerical abundance | 20 | 0 | 54 | 1 | 0 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
53.26 | 44-390A-5-41,126 | 0 | 50 | 50 | Lower eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 65 | 2 | 0 | 0 | 12 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
57.65 | 44-390A-6-1,25 | 0 | 20 | 40 | Lower eocene | NANNO OOZE | Dominat lithology; relative abundance | 30 | 2 | 62 | 5 | 0 | 0 | 2 | 1 | 3 | 2 | 2 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
57.65 | 44-390A-6-1,25 | 4 | 60 | 76 | Lower eocene | ZEOLITIC NANNO OOZE | Minor lithology; relative abundance | 0 | 0 | 77 | 8 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
59.65 | 44-390A-6-2,75 | 2 | 10 | 88 | Lower eocene | NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 80 | 1 | 0 | 0 | 1 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
61.15 | 44-390A-6-3,75 | 1 | 80 | 19 | Lower eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 55 | 5 | 0 | 0 | 10 | 5 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
62.40 | 44-390A-6-4,50 | 10 | 50 | 40 | Lower eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 37 | 5 | 0 | 0 | 10 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
64.41 | 44-390A-6-51,101 | 3 | 15 | 82 | Lower eocene | NANNO OOZE | Dominat lithology; relative abundance | 24 | 0 | 72 | 2 | 0 | 0 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
65.57 | 44-390A-6-6,67 | 2 | 70 | 28 | Lower eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 7 | 0 | 0 | 5 | 2 | 15 | 0 | 2 | 0 | 5 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
67.35 | 44-390A-7-1,85 | 0 | 75 | 25 | Lower eocene | NANNOFOSSIL OOZE | Dominat lithology; relative abundance | 20 | 2 | 70 | 5 | 0 | 0 | 1 | 2 | 1 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
68.90 | 44-390A-7-2,90 | 1 | 60 | 19 | Lower eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 50 | 10 | 0 | 0 | 10 | 10 | 20 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
68.90 | 44-390A-7-2,90 | 5 | 80 | 35 | Lower eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 50 | 8 | 0 | 0 | 15 | 5 | 8 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
69.79 | 44-390A-7-3,29 | 10 | 60 | 30 | Lower eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 35 | 5 | 0 | 0 | 20 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 |
71.40 | 44-390A-7-4,40 | 7 | 65 | 28 | Lower eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 50 | 8 | 0 | 0 | 15 | 10 | 15 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
77.25 | 44-390A-8-11,125 | 0 | 60 | 40 | Upper paleocene | NANNO OOZE | Dominat lithology; relative abundance | 30 | 2 | 50 | 5 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
78.26 | 44-390A-8-2,76 | 5 | 60 | 35 | Upper paleocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 60 | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 13 | 3 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
79.70 | 44-390A-8-3,70 | 2 | 58 | 40 | Upper paleocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 45 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 |
80.90 | 44-390A-8-4,40 | 0 | 70 | 30 | Upper paleocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 3 | 0 | 74 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 15 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
81.40 | 44-390A-8-4,90 | 2 | 48 | 50 | Upper paleocene | MARLY ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 12 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 25 | 6 | 30 | 0 | 0 | 2 | 0 | 2 | 0 | 0 |
82.10 | 44-390A-8-CC,0 | 1 | 30 | 70 | Upper paleocene | CHALK | Dominat lithology; relative abundance | 40 | 0 | 70 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
86.60 | 44-390A-9-11,110 | 0 | 10 | 90 | Lower paleocene | ZEOLITIC MARLY NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 55 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
96.38 | 44-390A-10-1,98 | 2 | 38 | 60 | Lower paleocene | ZEOLITIC MARLY NANNO OOZE | Dominat lithology; relative abundance | 2 | 2 | 66 | 4 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 15 | 2 | 13 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
96.45 | 44-390A-10-11,105 | 0 | 30 | 70 | Lower paleocene | ZEOLITIC MARLY NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 58 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 15 | 0 | 17 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
97.65 | 44-390A-10-2,75 | 5 | 60 | 35 | Lower paleocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 55 | 6 | 0 | 0 | 3 | 0 | 0 | 0 | 5 | 0 | 20 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
99.02 | 44-390A-10-3,62 | 1 | 0 | 0 | Lower paleocene | ZEOLITIC? MARLY NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 40 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 20 | 2 | 20 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
100.90 | 44-390A-10-41,100 | 0 | 25 | 75 | Lower paleocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
102.15 | 44-390A-10-5,75 | 1 | 25 | 75 | Lower paleocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
103.65 | 44-390A-10-6,75 | 1 | 50 | 50 | Lower paleocene | MARLY ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 2 | 25 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
104.50 | 44-390A-10-CC,0 | 1 | 40 | 60 | Lower paleocene | SILTY NANNO OOZE | Dominat lithology; relative abundance | 40 | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
106.75 | 44-390A-11-2,75 | 0 | 25 | 75 | Lower paleocene | NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 80 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 3 | 2 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
107.75 | 44-390A-11-3,25 | 1 | 40 | 60 | Lower paleocene | MARLY NANNO OOZE | Dominat lithology; relative abundance | 7 | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 40 | 0 | 0 | 2 | 2 | 0 | 0 | 0 |
109.75 | 44-390A-11-4,75 | 1 | 30 | 70 | Lower paleocene | MARLY NANNO OOZE | Dominat lithology; relative abundance | 15 | 2 | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 52 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
110.25 | 44-390A-11-41,125 | 1 | 40 | 60 | Lower paleocene | MARLY NANNO OOZE | Minor lithology; relative abundance | 10 | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 38 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
110.91 | 44-390A-11-5,41 | 1 | 20 | 80 | Lower paleocene | CALCAREOUS CLAY | Dominat lithology; relative abundance | 10 | 2 | 18 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 1 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
111.23 | 44-390A-11-5,73 | 0 | 30 | 70 | Lower paleocene | MARLY NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 36 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 2 | 34 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
111.74 | 44-390A-11-51,124 | 1 | 30 | 70 | Lower paleocene | MARLY NANNO OOZE | Dominat lithology; numerical abundance | 20 | 0 | 20 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 2 | 51 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
111.95 | 44-390A-11-51,145 | 1 | 50 | 50 | Lower paleocene | MARLY CALCAREOUS OOZE | Dominat lithology; relative abundance | 50 | 2 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
112.60 | 44-390A-11-6,60 | 0 | 40 | 60 | Upper maestrichtian | MARLY NANNO OOZE | Dominat lithology; relative abundance | 12 | 0 | 57 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 2 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
112.62 | 44-390A-11-6,62 | 0 | 40 | 60 | Upper maestrichtian | MARLY NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 65 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 3 | 2 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
113.60 | 44-390A-11-CC,0 | 1 | 60 | 40 | Upper maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 80 | 4 | 0 | 0 | 5 | 0 | 1 | 3 | 3 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
115.20 | 44-390A-12-1,75 | 1 | 40 | 60 | Upper maestrichtian | MARLY OOZE | Dominat lithology; relative abundance | 5 | 0 | 57 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 2 | 25 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
116.46 | 44-390A-12-2,51 | 0 | 30 | 70 | Upper maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 60 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
118.45 | 44-390A-12-31,100 | 0 | 40 | 60 | Upper maestrichtian | MARLY OOZE | Dominat lithology; relative abundance | 5 | 0 | 55 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 2 | 30 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
119.75 | 44-390A-12-4,80 | 0 | 40 | 60 | Upper maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 8 | 0 | 70 | 2 | 0 | 0 | 2 | 0 | 2 | 0 | 5 | 0 | 2 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
121.45 | 44-390A-12-51,100 | 0 | 40 | 60 | Upper maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 3 | 0 | 77 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 1 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
122.95 | 44-390A-12-61,100 | 0 | 30 | 70 | Upper maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 52 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 18 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
123.55 | 44-390A-12-CC,0 | 0 | 1 | 100 | Upper maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 85 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
124.63 | 44-390A-13-1,73 | 0 | 30 | 70 | Upper maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 30 | 0 | 44 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 1 | 24 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
126.17 | 44-390A-13-2,77 | 0 | 30 | 70 | Lower maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 2 | 0 | 2 | 0 | 0 | 0 | 0 |
127.40 | 44-390A-13-3,50 | 1 | 40 | 60 | Lower maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 9 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
129.40 | 44-390A-13-41,100 | 0 | 40 | 60 | Lower maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 60 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 19 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
130.65 | 44-390A-13-5,75 | 2 | 40 | 60 | Lower maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 7 | 0 | 76 | 9 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 2 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
132.30 | 44-390A-13-6,90 | 0 | 40 | 60 | Lower maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 70 | 8 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 2 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
133.00 | 44-390A-13-CC,0 | 0 | 1 | 100 | Lower maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 80 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
133.59 | 44-390A-14-1,59 | 0 | 40 | 60 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 30 | 0 | 55 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
135.80 | 44-390A-14-21,130 | 1 | 15 | 18 | Upper senonian | NANNO OOZE | Dominat lithology; numerical abundance | 30 | 0 | 62 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
136.40 | 44-390A-14-3,40 | 1 | 5 | 95 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 90 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
139.92 | 44-390A-14-5,92 | 0 | 40 | 60 | Albian | MARLY NANNO OOZE | Dominat lithology; relative abundance | 32 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 26 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
140.05 | 44-390A-14-51,105 | 0 | 5 | 95 | Albian | MARLY NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 61 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 28 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
140.60 | 44-390A-14-CC,0 | 0 | 10 | 10 | Albian | NANNO OOZE | Dominat lithology; numerical abundance | 19 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |