Müller, German; Stoffers, Peter (1974): (Table 3) Carbonate, quartz, and feldspar in different grain-size intervals of River Kizil Irmak draining into Black Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.400775, In supplement to: Müller, G; Stoffers, P (1974): Mineralogy and petrology of Black Sea basin sediments. The Black Sea - Geology, Chemistry, and Biology. Memoir. The American Association of Petroleum Geologists, 20, 200-248
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Project(s):
Funding:
Sixth Framework Programme (FP6), grant/award no. 36949: Southern European Seas: Assessing and Modelling Ecosystem Changes
Coverage:
Latitude: 41.290000 * Longitude: 35.550000
Minimum Elevation: 47.0 m * Maximum Elevation: 47.0 m
Event(s):
Inozu (804) * Latitude: 41.290000 * Longitude: 35.550000 * Elevation: 47.0 m * Location: Kizilirmak, Turkey, Asia * Campaign: Global River Discharge * Method/Device: River gauging station (RGS) * Comment: Area: 75121 km**2; Mapcode of UNESCO report: B4
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Size fraction | Size fraction | Müller, German | |||
| 2 | Carbonates | Carb | % | Müller, German | ||
| 3 | Calcite/Dolomite ratio | Cal/dol | Müller, German | |||
| 4 | Quartz | Qz | % | Müller, German | ||
| 5 | Feldspar | Fsp | % | Müller, German | ||
| 6 | Quartz/Feldspar ratio | Qz/Fsp | Müller, German | Calculated | ||
| 7 | Plagioclase/Kalifeldspar ratio | Pl/Kfs | Müller, German |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
63 data points
Data
| 1 Size fraction | 2 Carb [%] | 3 Cal/dol | 4 Qz [%] | 5 Fsp [%] | 6 Qz/Fsp | 7 Pl/Kfs |
|---|---|---|---|---|---|---|
| 707-500 | 8.0 | >10 | 48.4 | 13.6 | 3.55 | 2.8 |
| 500-354 | 4.0 | >10 | 36.2 | 33.1 | 1.09 | 1.5 |
| 354-250 | 7.5 | >10 | 23.5 | 32.3 | 0.72 | 1.1 |
| 250-177 | 11.0 | >10 | 24.6 | 42.6 | 0.58 | 1.2 |
| 177-125 | 11.5 | >10 | 24.2 | 56.3 | 0.42 | 6.2 |
| 125-88 | 10.0 | >10 | 31.1 | |||
| 88-63 | 12.0 | >12 | 33.0 | |||
| 63-20 | 12.0 | >10 | 28.0 | 0.70 | ||
| 20-6.3 | 11.0 | >10 | 27.0 | 0.90 | ||
| 6.3-2 | 11.0 | >10 | 21.0 | 1.00 | ||
| <2 | 15.0 | >10 | 17.0 | 1.00 |