Froget, C; Desprairies, Alain; Latouche, Claude; Maillet, Noelle (1989): (Table 5) Mineralogy of ODP Hole 104-642B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.735697, In supplement to: Froget, C et al. (1989): Paleoenvironmental significance of Cenozoic clay deposits from the Norwegian Sea: ODP Leg 104. In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 41-60, https://doi.org/10.2973/odp.proc.sr.104.112.1989
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 67.225000 * Longitude: 2.928300
Date/Time Start: 1985-06-28T14:40:00 * Date/Time End: 1985-06-29T20:15:00
Minimum DEPTH, sediment/rock: 2.14 m * Maximum DEPTH, sediment/rock: 216.88 m
Event(s):
104-642B * Latitude: 67.225000 * Longitude: 2.928300 * Date/Time Start: 1985-06-28T14:40:00 * Date/Time End: 1985-06-29T20:15:00 * Elevation: -1294.0 m * Penetration: 221.1 m * Recovery: 214.61 m * Location: Norwegian Sea * Campaign: Leg104 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 25 cores; 221.1 m cored; 0 m drilled; 97.1 % recovery
Comment:
<1 = trace, T = trace, P = present, - = absent
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Froget, C | DSDP/ODP/IODP sample designation | ||
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | Calcite | Cal | % | Froget, C | X-ray diffraction (XRD) | bulk sediment |
4 | Quartz | Qz | % | Froget, C | X-ray diffraction (XRD) | bulk sediment |
5 | Feldspar | Fsp | % | Froget, C | X-ray diffraction (XRD) | bulk sediment |
6 | Chlorite | Chl | % | Froget, C | X-ray diffraction, clay fraction | <2 µm, clay minerals |
7 | Illite | Ill | % | Froget, C | X-ray diffraction, clay fraction | <2 µm, clay minerals |
8 | Clay minerals | Clay min | % | Froget, C | X-ray diffraction, clay fraction | <2 µm, clay minerals, interlayer |
9 | Smectite | Sme | % | Froget, C | X-ray diffraction, clay fraction | <2 µm, clay minerals |
10 | Kaolinite | Kln | % | Froget, C | X-ray diffraction, clay fraction | <2 µm, clay minerals |
11 | Quartz | Qz | Froget, C | X-ray diffraction, clay fraction | <2 µm, associated minerals | |
12 | Feldspar | Fsp | Froget, C | X-ray diffraction, clay fraction | <2 µm, associated minerals | |
13 | Amphibole | Amp | Froget, C | X-ray diffraction, clay fraction | <2 µm, associated minerals | |
14 | Silica, amorphous | ASi | Froget, C | X-ray diffraction, clay fraction | <2 µm, associated minerals | |
15 | Opal-CT | Opal-CT | Froget, C | X-ray diffraction, clay fraction | <2 µm, associated minerals |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
336 data points
Data
1 Sample label | 2 Depth sed [m] | 3 Cal [%] | 4 Qz [%] | 5 Fsp [%] | 6 Chl [%] | 7 Ill [%] | 8 Clay min [%] | 9 Sme [%] | 10 Kln [%] | 11 Qz | 12 Fsp | 13 Amp | 14 ASi | 15 Opal-CT |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
104-642B-1H-2,67-69 | 2.14 | 12 | 16 | 27 | 15 | 28 | 5 | 37 | 15 | T | T | T | - | - |
104-642B-2H-3, 50-52 | 8.30 | 25 | 12 | 21 | 10 | 30 | 10 | 40 | 10 | T | T | T | - | - |
104-642B-3H-3,84-86 | 18.14 | 12 | 22 | 32 | 13 | 30 | 5 | 37 | 15 | T | T | T | - | - |
104-642B-5H-3,56-58 | 32.96 | 0 | 26 | 32 | 10 | 25 | 5 | 50 | 10 | T | T | T | - | - |
104-642B-6H-3,70-72 | 42.60 | 0 | 26 | 31 | 10 | 20 | 5 | 55 | 10 | T | T | T | - | - |
104-642B-7H-3,92-94 | 51.32 | 0 | 16 | 31 | 13 | 35 | 10 | 32 | 10 | - | T | T | - | - |
104-642B-8H-3,95-97 | 60.85 | 0 | 26 | 30 | 10 | 31 | 10 | 41 | 8 | T | T | T | - | - |
104-642B-9H-3,60-62 | 70.00 | 50 | 2 | 5 | 5 | 24 | 10 | 48 | 13 | - | - | - | - | - |
104-642B-10H-3,80-82 | 79.70 | 38 | 5 | <1 | 5 | 15 | 5 | 65 | 10 | - | - | - | T | - |
104-642B-11H-3,78-80 | 89.18 | 16 | 8 | 15 | 3 | 15 | 5 | 62 | 15 | - | - | - | T | - |
104-642B-12H-3,77-79 | 98.67 | 0 | 12 | 18 | 5 | 14 | 5 | 61 | 15 | - | - | - | T | - |
104-642B-13H-3,53-55 | 107.73 | 23 | 6 | 10 | 5 | 15 | 5 | 60 | 15 | - | - | - | T | - |
104-642B-14H-1,42-44 | 114.42 | 0 | 4 | 12 | 5 | 24 | 5 | 51 | 15 | - | - | - | T | - |
104-642B-15H-3,48-50 | 126.98 | 15 | 8 | 9 | 5 | 20 | 5 | 55 | 15 | - | - | - | T | - |
104-642B-16H-3,60-62 | 131.70 | 6 | 12 | 8 | 5 | 21 | 5 | 51 | 18 | - | - | - | T | - |
104-642B-17H-3,54-56 | 141.54 | 8 | 6 | <1 | 5 | 15 | 5 | 63 | 12 | - | - | - | T | - |
104-642B-18H-3,87-89 | 151.67 | 5 | 9 | 10 | 5 | 25 | 5 | 50 | 15 | - | - | - | T | - |
104-642B-19H-3,85-87 | 161.55 | 0 | 8 | 10 | 5 | 20 | 5 | 52 | 18 | - | - | - | T | - |
104-642B-20H-1,85-87 | 168.25 | 0 | 8 | 9 | 7 | 20 | 5 | 48 | 20 | - | - | - | T | - |
104-642B-21H-3,53-55 | 180.63 | 0 | 6 | 25 | 6 | 17 | 5 | 55 | 17 | - | - | - | T | - |
104-642B-22H-3,77-80 | 190.47 | 0 | 6 | <1 | 5 | 20 | 5 | 52 | 18 | - | - | - | T | - |
104-642B-23H-3,78-80 | 199.78 | 0 | 8 | 10 | <1 | 25 | 5 | 50 | 20 | - | - | - | T | - |
104-642B-24H-3,78-81 | 209.38 | 0 | 5 | <1 | 8 | 25 | 5 | 52 | 10 | - | - | - | T | - |
104-642B-25H-3,78-81 | 216.88 | 0 | 4 | <1 | 5 | 21 | 5 | 54 | 15 | - | - | - | T | - |