Kosheleva, Vera A; Bondarev, Vladimir N (2008): Light mineral composition of 0.100-0.050 mm grain size fraction of sediments from Hole AMIGE-1993-219 drilled in the Barents Sea [dataset]. All-Russian Research Institute for Geology and Mineral Resources of the World Ocean, St. Petersburg, PANGAEA, https://doi.org/10.1594/PANGAEA.676847, In: Kosheleva, VA; Bondarev, VN (1993): Processing results from drill hole AMIGE-1993-219 drilled in the Barents Sea, Central Rise (Murmansk) [dataset publication series]. All-Russian Research Institute for Geology and Mineral Resources of the World Ocean, St. Petersburg, PANGAEA, https://doi.org/10.1594/PANGAEA.688741
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 74.916700 * Longitude: 41.333300
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 19.00 m
Event(s):
AMIGE-1993-219 * Latitude: 74.916700 * Longitude: 41.333300 * Elevation: -150.0 m * Recovery: 19 m * Location: Barents Sea * Campaign: AMIGE-1993 * Method/Device: Drilling/drill rig (DRILL)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, top/min | Depth top | m | Kosheleva, Vera A | ||
| 3 | Depth, bottom/max | Depth bot | m | Kosheleva, Vera A | ||
| 4 | Sediment type | Sediment | Kosheleva, Vera A | |||
| 5 | Epoch | Epoch | Kosheleva, Vera A | |||
| 6 | Quartz | Qz | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 7 | Feldspar | Fsp | % | Kosheleva, Vera A | Counting, Stereo Microscope | K-Na feldspars |
| 8 | Plagioclase, acid | Pl acid | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 9 | Plagioclase | Pl | % | Kosheleva, Vera A | Counting, Stereo Microscope | middle |
| 10 | Micaceous-clayey aggregates | Mica-clay aggr | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 11 | Quartz-silica aggregates | Qz-Sil aggr | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 12 | Quartzite | Qzite | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 13 | Glauconite | Glt | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 14 | Calcite, organic | Cal org | Kosheleva, Vera A | Counting, Stereo Microscope | ||
| 15 | Calcite, inorganic | Cal inorg | Kosheleva, Vera A | Counting, Stereo Microscope | ||
| 16 | Obsidian | Obs | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 17 | Rock fragments | Rock fragm | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 18 | Muscovite | Ms | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 19 | Biotite | Bt | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 20 | Chlorite | Chl | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 21 | Iron hydroxides | Fe hydrx | % | Kosheleva, Vera A | Counting, Stereo Microscope | |
| 22 | Sum | Sum | % | Kosheleva, Vera A | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
630 data points
Data
| 1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Sediment | 5 Epoch | 6 Qz [%] | 7 Fsp [%] | 8 Pl acid [%] | 9 Pl [%] | 10 Mica-clay aggr [%] | 11 Qz-Sil aggr [%] | 12 Qzite [%] | 13 Glt [%] | 14 Cal org | 15 Cal inorg | 16 Obs [%] | 17 Rock fragm [%] | 18 Ms [%] | 19 Bt [%] | 20 Chl [%] | 21 Fe hydrx [%] | 22 Sum [%] |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.10 | 0.00 | 0.20 | clayey mud | Holocene | 24.8 | 13.0 | 0.9 | 0.3 | 59.1 | 0.4 | 0.3 | 0.0 | 0.3 | 0.1 | 0.0 | 0.1 | 0.1 | 0.3 | 0.3 | 0.0 | 100.0 |
| 0.50 | 0.40 | 0.60 | clayey mud | Holocene | 24.0 | 13.0 | 0.8 | 0.3 | 59.0 | 0.5 | 0.3 | 0.2 | 0.3 | 0.2 | 0.0 | 0.2 | 0.3 | 0.4 | 0.3 | 0.2 | 100.0 |
| 1.00 | 0.90 | 1.10 | clayey mud | Holocene | 24.9 | 13.2 | 0.9 | 0.3 | 58.0 | 0.5 | 0.3 | 0.2 | 0.3 | 0.2 | 0.0 | 0.2 | 0.2 | 0.3 | 0.3 | 0.2 | 100.0 |
| 1.30 | 1.20 | 1.40 | clayey mud | Holocene | 24.2 | 12.8 | 0.9 | 0.3 | 59.0 | 0.5 | 0.3 | 0.2 | 0.3 | 0.2 | 0.0 | 0.2 | 0.2 | 0.3 | 0.3 | 0.3 | 100.0 |
| 1.70 | 1.80 | 1.90 | clay | Holocene | 54.0 | 24.0 | 5.7 | 0.2 | 5.2 | 9.5 | 0.5 | 0.0 | 0 | 0 | 0.0 | 0.2 | 0.0 | 0.2 | 0.3 | 0.2 | 100.0 |
| 2.00 | 1.90 | 2.10 | clay | Holocene | 54.0 | 24.0 | 5.7 | 0.2 | 5.2 | 9.8 | 0.5 | 0.2 | 0 | 0 | 0.0 | 0.2 | 0.0 | 0.2 | 0.0 | 0.0 | 100.0 |
| 2.20 | 2.10 | 2.30 | clay | Holocene | 55.0 | 24.0 | 5.7 | 0.2 | 5.1 | 8.0 | 0.5 | 0.2 | 0.2 | 0 | 0.0 | 0.2 | 0.2 | 0.2 | 0.3 | 0.2 | 100.0 |
| 3.00 | 2.90 | 3.10 | clay | Holocene | 55.0 | 24.0 | 5.7 | 0.2 | 5.1 | 7.8 | 0.5 | 0.2 | 0.2 | 0.2 | 0.0 | 0.2 | 0.2 | 0.2 | 0.3 | 0.2 | 100.0 |
| 4.00 | 3.90 | 4.10 | clay | Holocene | 55.0 | 24.2 | 5.7 | 0.2 | 5.0 | 7.9 | 0.5 | 0.2 | 0 | 0.2 | 0.0 | 0.2 | 0.2 | 0.2 | 0.3 | 0.2 | 100.0 |
| 4.70 | 4.60 | 4.80 | clay | Holocene | 55.0 | 24.2 | 5.5 | 0.2 | 5.0 | 7.9 | 0.5 | 0.2 | 0.2 | 0.2 | 0.0 | 0.2 | 0.2 | 0.2 | 0.3 | 0.2 | 100.0 |
| 5.00 | 4.90 | 5.10 | clay | Holocene | 55.3 | 24.2 | 5.5 | 0.2 | 5.3 | 7.7 | 0.5 | 0.2 | 0.2 | 0 | 0.0 | 0.2 | 0.2 | 0.2 | 0.3 | 0.0 | 100.0 |
| 5.70 | 5.60 | 5.80 | clay | Holocene | 55.3 | 24.2 | 5.5 | 0.2 | 5.2 | 7.8 | 0.5 | 0.2 | 0.2 | 0 | 0.0 | 0.2 | 0.2 | 0.2 | 0.1 | 0.2 | 100.0 |
| 6.00 | 5.90 | 6.10 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.2 | 0.2 | 0.3 | 0.3 | 1.3 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 7.00 | 6.90 | 7.10 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.2 | 0.2 | 0.3 | 0.3 | 1.3 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 8.00 | 7.90 | 8.10 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.2 | 0.2 | 0.3 | 0.3 | 1.3 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 9.00 | 8.90 | 9.10 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.2 | 0.2 | 0.3 | 0.3 | 1.3 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 10.00 | 9.90 | 10.10 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.2 | 0.2 | 0.3 | 0.3 | 1.3 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 11.00 | 10.90 | 11.10 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.2 | 0.2 | 0.3 | 0.3 | 1.3 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 11.30 | 11.20 | 11.40 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.2 | 0.2 | 0.3 | 0.0 | 1.6 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 12.00 | 11.90 | 12.10 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.0 | 1.5 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 12.50 | 12.40 | 12.60 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 12.60 | 12.50 | 12.70 | clay (moraine ?) | Pleistocene | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 13.00 | 12.90 | 13.10 | clayey silt | Pleistocene ? | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 14.00 | 13.90 | 14.10 | clayey silt | Pleistocene ? | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 14.60 | 14.50 | 14.70 | clayey silt | Pleistocene ? | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 15.00 | 14.90 | 15.10 | clayey silt | Pleistocene ? | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 16.00 | 15.90 | 16.10 | clayey silt | Pleistocene ? | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 17.00 | 16.90 | 17.10 | clayey silt | Pleistocene ? | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 18.00 | 17.90 | 18.10 | clayey silt | Pleistocene ? | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |
| 19.00 | 18.90 | 19.10 | clayey silt | Pleistocene ? | 62.0 | 15.0 | 7.7 | 0.3 | 7.0 | 2.2 | 0.3 | 0.3 | 0.2 | 0.3 | 0.3 | 1.2 | 0.3 | 2.3 | 0.3 | 0.3 | 100.0 |