Perch-Nielsen, Katharina; Supko, Peter R (2005): Smear slide analysis of Hole 39-358 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230678
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
Perch-Nielsen, Katharina; Supko, Peter R; Boersma, Anne; Bonatti, Enrico; Carlson, Richard L; McCoy, Floyd W; Neprochnov, Yuri P; Zimmerman, H B (1977): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XXXIX, 1139 pp, https://doi.org/10.2973/dsdp.proc.39.1977
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -37.655200 * Longitude: -35.963700
Date/Time Start: 1974-11-30T00:00:00 * Date/Time End: 1974-11-30T00:00:00
Minimum DEPTH, sediment/rock: 48.89 m * Maximum DEPTH, sediment/rock: 820.10 m
Event(s):
39-358 * Latitude: -37.655200 * Longitude: -35.963700 * Date/Time: 1974-11-30T00:00:00 * Elevation: -4962.0 m * Penetration: 826.5 m * Recovery: 93.3 m * Location: South Atlantic/BASIN * Campaign: Leg39 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 152 m cored; 0 m drilled; 61.4 % 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 | Authigenic silica | Auth silica | % | Smear slide analysis | ||
14 | Radiolarians | Rad | % | Smear slide analysis | ||
15 | Diatoms | Diatoms | % | 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 | 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 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1371 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 Auth silica [%] | 14 Rad [%] | 15 Diatoms [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Mica [%] | 21 Clay min [%] | 22 Glt [%] | 23 Opaque [%] | 24 Py [%] | 25 Fe [%] | 26 Lm [%] | 27 HM [%] | 28 Volc glass [%] | 29 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
48.89 | 39-358-1-1,99 | 0 | 10 | 90 | Upper pleistocene | DIATOM MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 5 | 35 | 5 | 2 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 |
49.35 | 39-358-1-11,145 | 0 | 25 | 75 | Upper pleistocene | VOLCANIC MUD | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 40 | 0 | 0 | 0 | 30 | 0 | 0 | 1 | 0 | 1 | 2 | 20 | 0 |
52.96 | 39-358-1-4,56 | 0 | 20 | 80 | Upper pleistocene | BIO-SILICEOUS MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 15 | 20 | 5 | 8 | 5 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
54.53 | 39-358-1-5,63 | 0 | 10 | 90 | Lower pleistocene | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 5 | 10 | 0 | 1 | 2 | 65 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 |
54.77 | 39-358-1-5,87 | 0 | 10 | 90 | Lower pleistocene | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 5 | 10 | 5 | 17 | 5 | 0 | 2 | 55 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 |
123.76 | 39-358-2-1,26 | 0 | 0 | 0 | Upper miocene | MUD | Minor lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 20 | 5 | 5 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 40 | 0 | 0 | 0 | 10 | 0 |
124.53 | 39-358-2-11,103 | 0 | 10 | 90 | Upper miocene | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 5 | 15 | 5 | 5 | 0 | 0 | 2 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
125.60 | 39-358-2-2,60 | 0 | 10 | 90 | Upper miocene | BIO-SILICEOUS MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 8 | 10 | 5 | 5 | 0 | 8 | 0 | 65 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 |
202.30 | 39-358-3-2,80 | 0 | 20 | 80 | Miocene | SILICEOUS MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 10 | 5 | 5 | 0 | 35 | 0 | 0 | 5 | 0 | 2 | 2 | 10 | 0 |
203.50 | 39-358-3-3,50 | 0 | 0 | 0 | Miocene | SILICEOUS MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 10 | 10 | 5 | 0 | 40 | 0 | 4 | 0 | 0 | 0 | 0 | 5 | 0 |
207.36 | 39-358-3-51,136 | 0 | 15 | 85 | Miocene | VOLCANIC MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 15 | 2 | 10 | 2 | 60 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
276.81 | 39-358-4-11,131 | 0 | 10 | 90 | Lower miocene | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 35 | 5 | 10 | 5 | 2 | 5 | 0 | 20 | 2 | 0 | 5 | 0 | 2 | 1 | 15 | 0 |
278.21 | 39-358-4-21,121 | 0 | 30 | 70 | Lower miocene | RAD DIATOM MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 35 | 15 | 10 | 2 | 2 | 5 | 2 | 50 | 2 | 0 | 2 | 1 | 2 | 1 | 10 | 0 |
353.25 | 39-358-5-2,25 | 0 | 25 | 75 | Tertiary | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 30 | 5 | 15 | 2 | 0 | 5 | 0 | 25 | 0 | 0 | 5 | 0 | 0 | 0 | 15 | 0 |
353.90 | 39-358-5-2,90 | 0 | 35 | 65 | Tertiary | VOLCANIC-RICH RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 30 | 2 | 20 | 2 | 0 | 5 | 2 | 20 | 2 | 0 | 2 | 0 | 0 | 0 | 25 | 0 |
421.20 | 39-358-6-3,20 | 0 | 30 | 70 | Upper oligocene | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 40 | 10 | 15 | 5 | 0 | 5 | 2 | 15 | 0 | 0 | 5 | 0 | 2 | 0 | 5 | 0 |
422.36 | 39-358-6-31,136 | 0 | 0 | 0 | Upper oligocene | RAD LIMESTONE | Dominat lithology; relative abundance | 45 | 0 | 0 | 0 | 0 | 20 | 5 | 10 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 2 | 0 | 0 | 0 | 5 | 0 |
486.75 | 39-358-7-2,75 | 0 | 5 | 95 | Upper oligocene | SILICEOUS MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 30 | 2 | 5 | 0 | 30 | 5 | 0 | 5 | 0 | 2 | 0 | 5 | 0 |
487.23 | 39-358-7-21,123 | 0 | 5 | 95 | Upper oligocene | PYRITE-RICH SILICEOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 47 | 0 | 0 | 0 | 20 | 10 | 0 | 20 | 0 | 2 | 0 | 5 | 0 |
487.27 | 39-358-7-21,127 | 0 | 5 | 95 | Upper oligocene | SILICEOUS MUD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 45 | 0 | 5 | 0 | 25 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
552.90 | 39-358-8-2,40 | 0 | 85 | 15 | Upper oligocene | LIMESTONE | Minor lithology; numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
556.50 | 39-358-8-41,100 | 0 | 5 | 95 | Upper oligocene | SILICEOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 35 | 10 | 5 | 2 | 30 | 2 | 0 | 10 | 0 | 2 | 0 | 10 | 0 |
557.35 | 39-358-8-5,35 | 0 | 95 | 5 | Upper oligocene | LIMESTONE | Minor lithology; numerical abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
590.11 | 39-358-9-11,111 | 0 | 0 | 0 | Oligocene | LIMESTONE | Minor lithology; numerical abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
590.12 | 39-358-9-11,112 | 0 | 0 | 0 | Oligocene | LIMESTONE? | Minor lithology; numerical abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
592.80 | 39-358-9-3,80 | 0 | 10 | 90 | Oligocene | SILICEOUS MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 2 | 2 | 4 | 0 | 65 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 |
642.15 | 39-358-10-4,75 | 0 | 10 | 90 | Upper eocene | SILICEOUS MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 0 | 1 | 0 | 5 | 5 | 4 | 0 | 55 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 |
646.00 | 39-358-10-CC,0 | 0 | 0 | 0 | Upper eocene | PYRITIFEROUS MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 20 | 0 | 0 | 0 | 5 | 5 | 0 | 2 | 55 | 2 | 4 | 5 | 0 | 2 | 0 | 0 | 0 |
646.00 | 39-358-10-CC,0 | 0 | 0 | 0 | Upper eocene | SILICEOUS MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
704.66 | 39-358-11-2,16 | 0 | 0 | 0 | Middle eocene | SILICEOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 5 | 2 | 5 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
705.88 | 39-358-11-21,138 | 0 | 0 | 0 | Middle eocene | SILICEOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 28 | 5 | 5 | 0 | 55 | 2 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
706.94 | 39-358-11-3,94 | 0 | 10 | 90 | Middle eocene | SILICEOUS MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 14 | 0 | 30 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 60 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 1 |
707.48 | 39-358-11-31,148 | 0 | 10 | 90 | Middle eocene | PELAGIC CLAYSTONE | Minor lithology; numerical abundance | 0 | 5 | 0 | 0 | 15 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 80 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
707.50 | 39-358-11-31,150 | 0 | 10 | 90 | Middle eocene | PELAGIC CLAYSTONE | Minor lithology; relative abundance | 1 | 5 | 2 | 0 | 13 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
708.43 | 39-358-11-4,93 | 0 | 20 | 80 | Middle eocene | CHALK | Dominat lithology; relative abundance | 70 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
752.20 | 39-358-12-2,20 | 0 | 0 | 0 | Lower eocene | NANNO CHALK | Dominat lithology; numerical abundance | 40 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
752.40 | 39-358-12-2,40 | 0 | 0 | 0 | Lower eocene | FERRUGINOUS CALCAREOUS CHALK | Dominat lithology; relative abundance | 40 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 |
752.60 | 39-358-12-2,60 | 0 | 0 | 0 | Lower eocene | CALCAREOUS CHALK | Dominat lithology; relative abundance | 40 | 2 | 30 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
753.97 | 39-358-12-3,47 | 0 | 10 | 90 | Lower eocene | FERRUGINOUS MUD | Dominat lithology; relative abundance | 10 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 4 | 4 | 0 | 0 | 60 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 |
754.30 | 39-358-12-3,80 | 0 | 10 | 90 | Lower eocene | CHALK | Dominat lithology; numerical abundance | 60 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
784.20 | 39-358-13-4,70 | 0 | 10 | 90 | Middle paleocene | CHALK | Dominat lithology; relative abundance | 65 | 2 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
784.58 | 39-358-13-41,108 | 0 | 10 | 90 | Middle paleocene | FERRUGINOUS CHALK | Dominat lithology; numerical abundance | 25 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 15 | 0 | 0 | 0 | 13 | 0 | 0 | 0 | 0 |
793.10 | 39-358-14-4,10 | 0 | 0 | 0 | MARLY CHALK | Dominat lithology; relative abundance | 25 | 2 | 25 | 0 | 0 | 0 | 0 | 0 | 4 | 2 | 5 | 0 | 25 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | |
799.00 | 39-358-15-11,100 | 0 | 30 | 70 | Middle maestrichtian | FERRUGINOUS MUD | Dominat lithology; relative abundance | 0 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 15 | 5 | 10 | 0 | 50 | 0 | 0 | 0 | 15 | 0 | 1 | 1 | 0 |
800.90 | 39-358-15-21,140 | 0 | 10 | 90 | Middle maestrichtian | CHALK | Dominat lithology; relative abundance | 45 | 1 | 20 | 0 | 10 | 0 | 0 | 2 | 4 | 2 | 5 | 2 | 10 | 0 | 0 | 4 | 0 | 0 | 0 | 2 | 0 |
817.67 | 39-358-16-1,67 | 5 | 10 | 85 | Upper senonian | MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 25 | 10 | 1 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 4 | 2 | 1 |
819.30 | 39-358-16-2,80 | 0 | 10 | 90 | Upper senonian | CHALK | Dominat lithology; relative abundance | 50 | 2 | 20 | 0 | 10 | 0 | 0 | 0 | 5 | 5 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
820.10 | 39-358-16-CC,0 | 0 | 0 | 0 | Upper senonian | CALCAREOUS CHALK | Dominat lithology; numerical abundance | 40 | 0 | 10 | 5 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
820.10 | 39-358-16-CC,0 | 0 | 0 | 0 | Upper senonian | FERRUGINOUS MARLY CHALK | Dominat lithology; relative abundance | 60 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 |