Nürnberg, Dirk; Wollenburg, Ingo; Dethleff, Dirk; Eicken, Hajo; Kassens, Heidemarie; Letzig, Tom; Reimnitz, Erk; Thiede, Jörn (1994): (Table 3) Clay minerals in surface sediments from the Laptev Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.728652, In supplement to: Nürnberg, D et al. (1994): Sediments in Arctic sea ice: Implications for entrainment, transport and release. Marine Geology, 119(3-4), 185-214, https://doi.org/10.1016/0025-3227(94)90181-3
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Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Median Latitude: 76.874067 * Median Longitude: 135.631478 * South-bound Latitude: 76.000000 * West-bound Longitude: 133.083300 * North-bound Latitude: 77.800000 * East-bound Longitude: 140.066700
Minimum DEPTH, sediment/rock: 0 m * Maximum DEPTH, sediment/rock: 0 m
Comment:
data are given in peak area-%
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Nürnberg, Dirk | |||
| 2 | LATITUDE | Latitude | Geocode | |||
| 3 | LONGITUDE | Longitude | Geocode | |||
| 4 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 5 | Smectite | Sme | % | Nürnberg, Dirk | X-ray diffraction, calculated from peak area | |
| 6 | Illite | Ill | % | Nürnberg, Dirk | X-ray diffraction, calculated from peak area | |
| 7 | Chlorite | Chl | % | Nürnberg, Dirk | X-ray diffraction, calculated from peak area | |
| 8 | Kaolinite | Kln | % | Nürnberg, Dirk | X-ray diffraction, calculated from peak area |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
45 data points
Data
| 1 Sample label | 2 Latitude | 3 Longitude | 4 Depth sed [m] | 5 Sme [%] | 6 Ill [%] | 7 Chl [%] | 8 Kln [%] |
|---|---|---|---|---|---|---|---|
| 112-2 | 77.8000 | 140.0667 | 0 | 13 | 52 | 26 | 9 |
| 108-14 | 76.9833 | 134.9667 | 0 | 28 | 43 | 20 | 9 |
| 108-23 | 76.0000 | 133.0833 | 0 | 39 | 38 | 16 | 8 |
| 108-2 | 76.0000 | 133.0833 | 0 | 28 | 45 | 19 | 8 |
| 108-2b | 76.0000 | 133.0833 | 0 | 28 | 45 | 19 | 9 |
| 108-2 | 76.0000 | 133.0833 | 0 | 28 | 45 | 18 | 8 |
| 112-1 | 77.8000 | 140.0667 | 0 | 27 | 44 | 20 | 9 |
| 112-2 | 77.8000 | 140.0667 | 0 | 18 | 52 | 22 | 8 |
| 112-33 | 77.4833 | 133.1833 | 0 | 33 | 40 | 18 | 9 |