Froget, C; Desprairies, Alain; Latouche, Claude; Maillet, Noelle (1989): (Table 4) Mineralogy of ODP Hole 104-642C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.735698, 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: 67.220000 * Longitude: 2.930000
Date/Time Start: 1985-06-29T20:15:00 * Date/Time End: 1985-07-01T15:00:00
Minimum DEPTH, sediment/rock: 7.11 m * Maximum DEPTH, sediment/rock: 196.25 m
Event(s):
104-642C * Latitude: 67.220000 * Longitude: 2.930000 * Date/Time Start: 1985-06-29T20:15:00 * Date/Time End: 1985-07-01T15:00:00 * Elevation: -1292.0 m * Penetration: 199.6 m * Recovery: 194.93 m * Location: Norwegian Sea * Campaign: Leg104 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 199.6 m cored; 0 m drilled; 97.7 % 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:
294 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 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
104-642C-2H-3,71-73 | 7.11 | 5 | 18 | 27 | 15 | 35 | 5 | 31 | 14 | T | T | - | - | - |
104-642C-4H-3,77-79 | 26.87 | 10 | 19 | 38 | 15 | 36 | 5 | 29 | 15 | T | T | T | - | - |
104-642C-5H-3,78-80 | 36.68 | 6 | 22 | 22 | 15 | 38 | 10 | 27 | 10 | T | T | T | - | - |
104-642C-6H-3,78-80 | 45.18 | 0 | 26 | 28 | 15 | 30 | 10 | 30 | 15 | T | - | - | - | - |
104-642C-7H-3,19-21 | 54.09 | 0 | 42 | 26 | 5 | 25 | 10 | 45 | 15 | T | T | T | - | - |
104-642C-8H-3,19-21 | 60.29 | 0 | 13 | 22 | 12 | 25 | 10 | 40 | 13 | T | T | - | - | - |
104-642C-10H-3,66-68 | 67.16 | 43 | 5 | 8 | 10 | 20 | 5 | 60 | 5 | T | T | T | T | - |
104-642C-11H-3,48-50 | 76.66 | 38 | 4 | 11 | 15 | 33 | 5 | 30 | 17 | - | - | T | T | - |
104-642C-12H-3,50-52 | 86.00 | 0 | 10 | 14 | 5 | 18 | 5 | 57 | 15 | - | - | - | T | - |
104-642C-13H-3,35-37 | 96.35 | 0 | 12 | 15 | 5 | 20 | 5 | 55 | 15 | T | - | T | T | - |
104-642C-14H-3,49-51 | 104.99 | 18 | 7 | 13 | 3 | 18 | 5 | 60 | 14 | T | T | - | T | - |
104-642C-15H-3,59-51 | 114.59 | 0 | 10 | 13 | 4 | 16 | 5 | 60 | 15 | T | T | - | T | - |
104-642C-16H-3,47-49 | 123.97 | 0 | 7 | 10 | 3 | 18 | 5 | 60 | 14 | - | - | - | T | - |
104-642C-17H-3,80-83 | 133.80 | 32 | 4 | 0 | 5 | 13 | 5 | 64 | 13 | - | - | - | T | - |
104-642C-19H-3,71-73 | 152.71 | 0 | <1 | 7 | 2 | 14 | 5 | 64 | 15 | - | - | - | T | - |
104-642C-19H-3,83-86 | 152.83 | 15 | 3 | 5 | 5 | 24 | 5 | 55 | 11 | - | - | - | T | - |
104-642C-20H-3,78-81 | 162.28 | 0 | 8 | 9 | 5 | 20 | 5 | 55 | 15 | - | - | - | T | - |
104-642C-21H-3,84-87 | 171.84 | 0 | 6 | <1 | 7 | 16 | 5 | 56 | 16 | - | - | - | T | - |
104-642C-22H-3,85-88 | 181.35 | 0 | 5 | <1 | 4 | 16 | 5 | 60 | 15 | - | - | - | T | - |
104-642C-23H-3,85-88 | 188.15 | 0 | 2 | 10 | 4 | 18 | 5 | 58 | 15 | - | - | - | T | - |
104-642C-24H-3,85-87 | 196.25 | 0 | 2 | 6 | 5 | 20 | 5 | 55 | 15 | T | T | - | T | - |