Andreicheva, L N (2007): (Table 2) Petrographic composition of coarse clastic material from tills of the Shapkina River valley [dataset]. Institute of Geology, Komi Scientific Cener, Ural Division, Russian Academy of Sciences, PANGAEA, https://doi.org/10.1594/PANGAEA.784062, In supplement to: Andreicheva, LN (2007): Pleistocene sediments in the Shapkina River valley (Bol'shaya Zemlya Tundra). Translated from Litologiya i Poleznye Iskopaemye, 2007, 1, 93-110, Lithology and Mineral Resources, 42(1), 84-100, https://doi.org/10.1134/S0024490207010099
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 67.171818 * Median Longitude: 54.085455 * South-bound Latitude: 66.800000 * West-bound Longitude: 53.210000 * North-bound Latitude: 67.510000 * East-bound Longitude: 54.710000
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 | Outcrop | Outcrop | Andreicheva, L N | |||
| 5 | Horizon | Horizon | Andreicheva, L N | |||
| 6 | Limestone | Lmst | % | Andreicheva, L N | and dolomite; dark gray and black; Paleozoic | |
| 7 | Limestone | Lmst | % | Andreicheva, L N | light gray and white; Paleozoic | |
| 8 | Terrigenous | Terr | % | Andreicheva, L N | proximal; Jurassic and Lower Cretaceous | |
| 9 | Terrigenous | Terr | % | Andreicheva, L N | transitional; Permian and Triassic | |
| 10 | Metamorphite | Metam | % | Andreicheva, L N | and igneous rocks; distal | |
| 11 | Quartzite | Qzite | % | Andreicheva, L N | and quartzite sandstones; distal |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
144 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Outcrop | 5 Horizon | 6 Lmst [%] (and dolomite; dark gray and b...) | 7 Lmst [%] (light gray and white; Paleozoic) | 8 Terr [%] (proximal; Jurassic and Lower ...) | 9 Terr [%] (transitional; Permian and Tri...) | 10 Metam [%] (and igneous rocks; distal) | 11 Qzite [%] (and quartzite sandstones; distal) |
|---|---|---|---|---|---|---|---|---|---|---|
| ShRV-1 | 67.51 | 54.63 | 1a | Q4-III_p | 30.0 | 20.0 | 22.5 | 12.5 | 2.5 | 12.5 |
| ShRV-1 | 67.51 | 54.63 | 1c | Q4-II_vc | 1.8 | 22.8 | 15.4 | 22.7 | 30.1 | 7.2 |
| ShRV-2 | 67.46 | 54.71 | 2a | Q4-III_p | 26.0 | 17.5 | 14.8 | 13.5 | 12.4 | 15.8 |
| ShRV-3 | 67.46 | 54.50 | 1-Mar | Q4-II_vc | 12.0 | 28.0 | 22.0 | 18.0 | 8.0 | 12.0 |
| ShRV-4 | 67.40 | 54.46 | 4-Apr | Q4-II_vc | 16.5 | 22.0 | 19.8 | 17.5 | 17.6 | 6.6 |
| ShRV-4 | 67.40 | 54.46 | 6-Apr | Q4-II_vc | 15.7 | 23.6 | 17.6 | 16.7 | 15.4 | 11.0 |
| ShRV-6 | 67.30 | 54.30 | 6 | Q2-II_pc | 29.7 | 8.8 | 36.2 | 19.8 | 2.2 | 3.3 |
| ShRV-7 | 67.26 | 54.13 | 1-Jul | Q4-II_vc | 10.5 | 20.0 | 14.7 | 16.6 | 17.3 | 20.9 |
| ShRV-8 | 67.15 | 54.14 | 8 | Q4-II_vc | 3.0 | 22.0 | 24.0 | 14.0 | 29.0 | 8.0 |
| ShRV-10 | 66.92 | 53.66 | 10 | Q4-II_vc | 6.7 | 30.2 | 23.0 | 16.6 | 18.3 | 5.2 |
| ShRV-11 | 66.82 | 53.70 | 11 | Q4-II_vc | 5.5 | 30.7 | 18.7 | 14.2 | 19.9 | 11.0 |
| ShRV-12 | 66.80 | 53.50 | 1-Dec | Q4-II_vc | 14.8 | 31.8 | 20.4 | 12.8 | 8.0 | 12.4 |
| ShRV-12 | 66.80 | 53.50 | 2-Dec | Q4-II_vc | 17.1 | 30.6 | 20.8 | 13.5 | 7.2 | 10.8 |
| ShRV-12 | 66.80 | 53.50 | 6-Dec | Q4-II_vc | 17.4 | 26.1 | 21.7 | 14.5 | 8.7 | 11.6 |
| ShRV-12 | 66.80 | 53.50 | 12-pit | Q4-II_vc | 15.1 | 30.0 | 21.5 | 11.8 | 7.6 | 14.0 |
| ShRV-13 | 66.81 | 53.21 | 13-1 | Q4-II_vc | 8.8 | 29.4 | 22.1 | 16.2 | 16.2 | 7.3 |
| ShRV-13 | 66.81 | 53.21 | 13-2 | Q4-II_vc | 9.8 | 35.2 | 22.0 | 13.4 | 15.9 | 3.7 |
| ShRV-13 | 66.81 | 53.21 | 13-3 | Q4-III_p | 18.0 | 27.9 | 21.7 | 9.9 | 9.9 | 12.6 |