Shimkus, Kazimir M; Rozanov, Alexander G (1999): (Table 5) Contents of clay minerals in <0.002 mm grain size fraction of Upper Quaternary bottom sediments from the Latakian depression of the Mediterranean Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.760705, In supplement to: Shimkus, KM; Rozanov, AG (1999): Bottom sediments and Late Quaternary sedimentation in the Syrian region of the Mediterranean Sea. Translated from Okeanologiya, 1999, 39(3), 440-450, Oceanology, 39(3), 401-410
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 35.253950 * Median Longitude: 35.194300 * South-bound Latitude: 35.147900 * West-bound Longitude: 35.186100 * North-bound Latitude: 35.360000 * East-bound Longitude: 35.202500
Minimum DEPTH, sediment/rock: 0.0100 m * Maximum DEPTH, sediment/rock: 1.6750 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | Elevation of event | Elevation | m | |||
5 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
6 | Depth, top/min | Depth top | m | Shimkus, Kazimir M | ||
7 | Depth, bottom/max | Depth bot | m | Shimkus, Kazimir M | ||
8 | Kaolinite | Kln | % | Shimkus, Kazimir M | X-ray diffraction (XRD) | |
9 | Chlorite | Chl | % | Shimkus, Kazimir M | X-ray diffraction (XRD) | |
10 | Hydromica | Hydromica | % | Shimkus, Kazimir M | X-ray diffraction (XRD) | |
11 | Plagioclase | Pl | % | Shimkus, Kazimir M | X-ray diffraction (XRD) | |
12 | Montmorillonite | Mnt | % | Shimkus, Kazimir M | X-ray diffraction (XRD) | |
13 | Sum | Sum | % | Shimkus, Kazimir M | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
136 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Depth sed [m] | 6 Depth top [m] | 7 Depth bot [m] | 8 Kln [%] | 9 Chl [%] | 10 Hydromica [%] | 11 Pl [%] | 12 Mnt [%] | 13 Sum [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|
Vy27-3941 | 35.3600 | 35.2025 | -1060 | 0.0100 | 0.000 | 0.02 | 8 | 6 | 14 | 3 | 69 | 100 |
Vy27-3941 | 35.3600 | 35.2025 | -1060 | 0.1500 | 0.130 | 0.17 | 9 | 0 | 16 | 3 | 72 | 100 |
Vy27-3941 | 35.3600 | 35.2025 | -1060 | 0.2200 | 0.170 | 0.27 | 13 | 0 | 17 | 5 | 65 | 100 |
Vy27-3941 | 35.3600 | 35.2025 | -1060 | 0.4500 | 0.400 | 0.50 | 16 | 0 | 0 | 0 | 84 | 100 |
Vy27-3941 | 35.3600 | 35.2025 | -1060 | 0.6250 | 0.500 | 0.75 | 12 | 8 | 11 | 3 | 66 | 100 |
Vy27-3941 | 35.3600 | 35.2025 | -1060 | 0.8500 | 0.800 | 0.90 | 11 | 9 | 15 | 3 | 62 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 0.1500 | 0.100 | 0.20 | 11 | 0 | 17 | 7 | 65 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 0.3750 | 0.350 | 0.40 | 13 | 0 | 18 | 6 | 63 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 0.4400 | 0.400 | 0.48 | 12 | 0 | 18 | 0 | 70 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 0.5300 | 0.480 | 0.58 | 14 | 0 | 25 | 8 | 53 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 0.7300 | 0.680 | 0.78 | 14 | 0 | 16 | 0 | 70 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 0.8150 | 0.780 | 0.85 | 13 | 0 | 26 | 10 | 51 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 0.8800 | 0.850 | 0.91 | 8 | 0 | 10 | 3 | 79 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 0.9675 | 0.935 | 1.00 | 8 | 0 | 20 | 8 | 64 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 1.2500 | 1.200 | 1.30 | 14 | 9 | 10 | 4 | 63 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 1.3600 | 1.320 | 1.40 | 18 | 15 | 15 | 0 | 52 | 100 |
Vy27-4007 | 35.1479 | 35.1861 | -1210 | 1.6750 | 1.600 | 1.75 | 16 | 0 | 15 | 0 | 69 | 100 |