Benson, William E; Sheridan, Robert E (2005): Smear slide analysis of Hole 44-390 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230726
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: 1.28 m * Maximum DEPTH, sediment/rock: 189.60 m
Event(s):
44-390 * Latitude: 30.142300 * Longitude: -76.112300 * Date/Time: 1975-08-29T00:00:00 * Elevation: -2665.0 m * Penetration: 206 m * Recovery: 27.1 m * Location: North Atlantic Ocean * Campaign: Leg44 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 9 cores; 82.5 m cored; 9.5 m drilled; 32.9 % 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 | 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 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals | |
18 | Quartz | Qz | % | Smear slide analysis | ||
19 | Feldspar | Fsp | % | Smear slide analysis | ||
20 | Zeolite | Zeo | % | Smear slide analysis | ||
21 | Mica | Mica | % | Smear slide analysis | ||
22 | Clay minerals | Clay min | % | Smear slide analysis | ||
23 | Opaque minerals | Opaque | % | Smear slide analysis | ||
24 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
25 | Iron | Fe | % | Smear slide analysis | ||
26 | Limonite | Lm | % | Smear slide analysis | ||
27 | Heavy minerals | HM | % | Smear slide analysis | ||
28 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
29 | Palagonite | Palagonite | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1253 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 Minerals [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Clay min [%] | 23 Opaque [%] | 24 Py [%] | 25 Fe [%] | 26 Lm [%] | 27 HM [%] | 28 Volc glass [%] | 29 Palagonite [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.28 | 44-390-1-11,128 | 1 | 80 | 20 | Middle eocene | ZEOLITIC NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 70 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1.33 | 44-390-1-11,133 | 0 | 5 | 95 | Middle eocene | FORAMINIFERAL NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 70 | 10 | 2 | 2 | 2 | 0 | 0 | 2 | 0 | 10 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1.54 | 44-390-1-2,4 | 1 | 80 | 20 | Middle eocene | NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 80 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
2.18 | 44-390-1-2,68 | 0 | 10 | 90 | Middle eocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 85 | 5 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
2.48 | 44-390-1-2,98 | 2 | 88 | 10 | Middle eocene | NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 78 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
3.51 | 44-390-1-3,51 | 1 | 80 | 19 | Middle eocene | NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 85 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
4.90 | 44-390-1-4,40 | 78 | 20 | 2 | Middle eocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 10 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
5.53 | 44-390-1-41,103 | 0 | 0 | 0 | Middle eocene | OOZE | Dominat lithology; relative abundance | 10 | 0 | 80 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.80 | 44-390-1-5,80 | 0 | 1 | 100 | Middle eocene | OOZE | Dominat lithology; relative abundance | 20 | 0 | 78 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
7.60 | 44-390-1-6,10 | 0 | 5 | 95 | Middle eocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 75 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 10 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
8.66 | 44-390-1-61,116 | 1 | 80 | 20 | Middle eocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 70 | 10 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 15 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 2 | 0 |
9.10 | 44-390-1-CC,0 | 0 | 0 | 0 | Middle eocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 60 | 1 | 0 | 2 | 2 | 0 | 0 | 2 | 2 | 10 | 2 | 10 | 2 | 2 | 0 | 0 | 2 | 0 | 2 |
9.10 | 44-390-1-CC,0 | 0 | 70 | 20 | Middle eocene | NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 65 | 12 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 10 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
9.10 | 44-390-1-CC,0 | 0 | 80 | 30 | Middle eocene | ZEOLITES | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
124.89 | 44-390-2-11,139 | 0 | 1 | 100 | Upper maestrichtian | MARLY NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 24 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
133.85 | 44-390-3-1,85 | 0 | 20 | 80 | Cretaceous | NANNO OOZE | Dominat lithology; numerical abundance | 20 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
134.42 | 44-390-3-11,142 | 0 | 10 | 90 | Cretaceous | CALCAREOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 70 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
134.91 | 44-390-3-2,40.5 | 0 | 80 | 20 | Cretaceous | CALCAREOUS CLAY | Minor lithology; relative abundance | 2 | 0 | 20 | 2 | 0 | 0 | 0 | 15 | 0 | 30 | 0 | 0 | 3 | 25 | 0 | 0 | 5 | 0 | 2 | 0 | 0 |
134.92 | 44-390-3-2,42 | 1 | 5 | 95 | Cretaceous | CLAYEY OOZE | Minor lithology; relative abundance | 0 | 0 | 60 | 1 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 39 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
135.43 | 44-390-3-2,93 | 0 | 5 | 95 | Cretaceous | CLAY | Dominat lithology; relative abundance | 0 | 2 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 2 | 2 | 10 | 0 | 0 | 40 | 0 | 20 | 0 | 0 |
135.55 | 44-390-3-21,105 | 0 | 0 | 0 | Cretaceous | HARD NODULE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
136.71 | 44-390-3-3,71 | 0 | 1 | 100 | Cretaceous | MARLY NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 30 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 2 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.15 | 44-390-3-31,115 | 0 | 10 | 90 | Cretaceous | CLAY | Dominat lithology; relative abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 5 | 0 | 40 | 0 | 2 | 1 | 10 | 0 | 0 | 40 | 0 | 2 | 0 | 0 |
137.23 | 44-390-3-31,123 | 5 | 35 | 60 | Cretaceous | LIMESTONE | Minor lithology; relative abundance | 80 | 2 | 5 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
143.74 | 44-390-4-11,124 | 0 | 20 | 80 | Albian | CHALK | Minor lithology; relative abundance | 75 | 0 | 7 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 2 | 2 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
143.86 | 44-390-4-11,136 | 0 | 75 | 25 | Albian | MARLY NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 24 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
144.41 | 44-390-4-2,41 | 0 | 80 | 20 | Albian | CALCAREOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 35 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
145.09 | 44-390-4-21,109 | 1 | 40 | 60 | Albian | MARLY SILTY NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 25 | 2 | 0 | 0 | 0 | 0 | 0 | 20 | 2 | 0 | 2 | 50 | 0 | 0 | 0 | 0 | 2 | 2 | 0 |
145.29 | 44-390-4-21,129 | 2 | 20 | 78 | Albian | CLACAREOUS CLAY | Minor lithology; relative abundance | 0 | 0 | 15 | 2 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 2 | 5 | 65 | 0 | 3 | 0 | 2 | 2 | 0 | 0 |
145.60 | 44-390-4-CC,0 | 0 | 25 | 10 | Albian | LIMESTONE | Dominat lithology; relative abundance | 85 | 1 | 10 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 2 | 2 | 30 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
145.60 | 44-390-4-CC,0 | 0 | 90 | 75 | Albian | MARLY NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
152.80 | 44-390-5-1,80 | 60 | 40 | 60 | Upper aptian | MARLY NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 35 | 0 | 0 | 1 | 2 | 0 | 0 | 0 |
153.45 | 44-390-5-11,145 | 0 | 60 | 40 | Upper aptian | CHALK | Dominat lithology; numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
153.93 | 44-390-5-2,43 | 0 | 10 | 90 | Upper aptian | CHALK | Dominat lithology; relative abundance | 65 | 0 | 20 | 0 | 0 | 0 | 0 | 10 | 0 | 2 | 0 | 2 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
155.10 | 44-390-5-CC,0 | 0 | 80 | 20 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 95 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
162.50 | 44-390-6-11,100 | 1 | 20 | 80 | Lower cretaceous | LIME MUD | Dominat lithology; numerical abundance | 100 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
162.92 | 44-390-6-11,142 | 0 | 60 | 40 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 85 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
163.10 | 44-390-6-CC,0 | 0 | 50 | 40 | Lower cretaceous | CALCAREOUS MUD | Dominat lithology; numerical abundance | 100 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
163.10 | 44-390-6-CC,0 | 0 | 60 | 50 | Lower cretaceous | Dominat lithology; relative abundance | 95 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
186.25 | 44-390-8-41,125 | 0 | 60 | 40 | CHALK | Dominat lithology; numerical abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
187.06 | 44-390-8-5,56 | 0 | 80 | 20 | LIMESTONE OR CHALK? | Dominat lithology; relative abundance | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
187.20 | 44-390-8-5,70 | 0 | 30 | 70 | LIMESTONE | Dominat lithology; numerical abundance | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
189.28 | 44-390-8-61,128 | 0 | 90 | 10 | LIMESTONE | Dominat lithology; numerical abundance | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
189.60 | 44-390-8-CC,0 | 0 | 0 | 0 | CHALK | Dominat lithology; numerical abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
189.60 | 44-390-8-CC,0 | 0 | 80 | 20 | LIMESTONE-CHALK | Dominat lithology; numerical abundance | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |