Viscosi-Shirley, C; Mammone, K; Pisias, Nicklas G; Dymond, Jack R (2003): (Table 1) Clay mineral percentages in surface sediments from the Siberian Arctic shelf [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.132131, In supplement to: Viscosi-Shirley, C et al. (2003): Clay mineralogy and multi-element chemistry of surface sediments on the Siberian Arctic shelf: implications for sediment provenance and grain size sorting. Continental Shelf Research, 23(11-13), 1175-1200, https://doi.org/10.1016/S0278-4343(03)00091-8
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 72.236662 * Median Longitude: 154.991277 * South-bound Latitude: 67.470000 * West-bound Longitude: 120.000000 * North-bound Latitude: 76.433000 * East-bound Longitude: -170.370000
Date/Time Start: 1963-09-02T00:00:00 * Date/Time End: 1963-09-02T00:00:00
Minimum DEPTH, sediment/rock: 0 m * Maximum DEPTH, sediment/rock: 0 m
Event(s):
BI64-17 * Latitude: 72.400000 * Longitude: 157.500000 * Location: East Siberian Sea * Campaign: BI64 * Method/Device: Grab (GRAB)
NW63-14 * Latitude: 67.470000 * Longitude: -170.370000 * Location: Chukchi Sea * Campaign: NW63 * Basis: Northwind * Method/Device: Grab (GRAB)
NW63-18 * Latitude: 68.600000 * Longitude: -171.600000 * Location: Chukchi Sea * Campaign: NW63 * Basis: Northwind * Method/Device: Grab (GRAB)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Illite | Ill | % | Viscosi-Shirley, C | X-ray diffraction, clay fraction | |
| 4 | Chlorite | Chl | % | Viscosi-Shirley, C | X-ray diffraction, clay fraction | |
| 5 | Smectite | Sme | % | Viscosi-Shirley, C | X-ray diffraction, clay fraction | |
| 6 | Kaolinite | Kln | % | Viscosi-Shirley, C | X-ray diffraction, clay fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
260 data points
Data
| 1 Event | 2 Depth sed [m] | 3 Ill [%] | 4 Chl [%] | 5 Sme [%] | 6 Kln [%] |
|---|---|---|---|---|---|
| BI64-17 | 0 | 65 | 19 | 12 | 4 |
| NW362-62 | 0 | 49 | 24 | 26 | 2 |
| NW362-70 | 0 | 44 | 23 | 28 | 5 |
| NW63-101 | 0 | 61 | 23 | 9 | 7 |
| NW63-103 | 0 | 63 | 23 | 7 | 7 |
| NW63-107 | 0 | 62 | 24 | 8 | 6 |
| NW63-115 | 0 | 54 | 20 | 15 | 10 |
| NW63-118 | 0 | 53 | 20 | 18 | 10 |
| NW63-119 | 0 | 56 | 21 | 14 | 9 |
| NW63-122 | 0 | 59 | 22 | 10 | 9 |
| NW63-125 | 0 | 57 | 22 | 10 | 11 |
| NW63-128 | 0 | 53 | 20 | 17 | 10 |
| NW63-130 | 0 | 52 | 21 | 19 | 8 |
| NW63-134 | 0 | 54 | 20 | 16 | 10 |
| NW63-136 | 0 | 53 | 20 | 18 | 9 |
| NW63-139 | 0 | 53 | 20 | 19 | 8 |
| NW63-14 | 0 | 48 | 26 | 23 | 4 |
| NW63-141 | 0 | 50 | 21 | 18 | 11 |
| NW63-143 | 0 | 46 | 15 | 28 | 11 |
| NW63-146 | 0 | 49 | 17 | 24 | 9 |
| NW63-148 | 0 | 48 | 18 | 24 | 9 |
| NW63-149 | 0 | 48 | 21 | 25 | 6 |
| NW63-151 | 0 | 49 | 17 | 27 | 7 |
| NW63-153 | 0 | 47 | 17 | 26 | 10 |
| NW63-157 | 0 | 45 | 15 | 32 | 9 |
| NW63-160 | 0 | 44 | 14 | 32 | 10 |
| NW63-161 | 0 | 41 | 15 | 34 | 10 |
| NW63-166 | 0 | 35 | 16 | 39 | 10 |
| NW63-18 | 0 | 50 | 25 | 19 | 5 |
| NW63-188 | 0 | 44 | 17 | 30 | 9 |
| NW63-19 | 0 | 53 | 24 | 17 | 7 |
| NW63-193 | 0 | 52 | 19 | 20 | 9 |
| NW63-197 | 0 | 64 | 21 | 9 | 5 |
| NW63-21 | 0 | 52 | 19 | 23 | 6 |
| NW63-25 | 0 | 54 | 28 | 13 | 6 |
| NW63-26 | 0 | 48 | 25 | 20 | 7 |
| NW63-27 | 0 | 47 | 27 | 19 | 7 |
| NW63-28 | 0 | 54 | 21 | 21 | 4 |
| NW63-29 | 0 | 49 | 23 | 22 | 6 |
| NW63-32 | 0 | 57 | 24 | 14 | 6 |
| NW63-34 | 0 | 44 | 24 | 24 | 7 |
| NW63-37 | 0 | 50 | 22 | 21 | 7 |
| NW63-39 | 0 | 52 | 20 | 23 | 6 |
| NW63-40 | 0 | 55 | 22 | 19 | 4 |
| NW63-41 | 0 | 56 | 22 | 15 | 7 |
| NW63-42 | 0 | 55 | 20 | 19 | 6 |
| NW63-44 | 0 | 51 | 22 | 20 | 7 |
| NW63-46 | 0 | 62 | 21 | 13 | 3 |
| NW63-50 | 0 | 63 | 23 | 11 | 4 |
| NW63-51 | 0 | 67 | 23 | 6 | 4 |
| NW63-52 | 0 | 61 | 24 | 12 | 3 |
| NW63-54 | 0 | 63 | 23 | 10 | 4 |
| NW63-57 | 0 | 59 | 28 | 9 | 4 |
| NW63-60 | 0 | 61 | 24 | 11 | 4 |
| NW63-64 | 0 | 58 | 27 | 10 | 5 |
| NW63-67 | 0 | 64 | 24 | 7 | 5 |
| NW63-77 | 0 | 64 | 23 | 7 | 6 |
| NW63-80 | 0 | 64 | 21 | 10 | 5 |
| NW63-82 | 0 | 62 | 25 | 6 | 7 |
| NW63-87 | 0 | 62 | 22 | 9 | 7 |
| NW63-88 | 0 | 63 | 24 | 8 | 6 |
| NW63-94 | 0 | 56 | 27 | 8 | 8 |
| NW63-95 | 0 | 61 | 23 | 9 | 8 |
| NW63-97 | 0 | 57 | 25 | 10 | 8 |
| NW63-99 | 0 | 59 | 23 | 10 | 9 |