Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Jessica Yurevna; Vasil'chuk, Alla Constantinovna; Garankina, Ekaterina Vadimovna; Chizhova, Julia Nikolaevna; Shorkunov, Il'ya Germanovich (2020): The deposits sourrounding late Pleistocene massive ice bodies in the region of Bovanenkovskoye oil and gas condensate field [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.921679, In: Vasil'chuk, YK et al. (2020): Isotope-geochemical composition of the massive ice of the Mordyakha and Seyakha (Mutnaya) Rivers interfluve, Central Yamal Peninsula [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.921687
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Keyword(s):
Supplement to:
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Jessica Yurevna; Vasil'chuk, Alla Constantinovna; Garankina, Ekaterina Vadimovna; Chizhova, Julia Nikolaevna; Shorkunov, Il'ya Germanovich (2018): Isotope-geochemical composition of massive ice beddings on the interfluve of the rivers Mordyakha and Seyakha (Mutnaya), Central Yamal Peninsula. Arktika i Antarktika (Arctic and Antarctic), 1, 50-75, https://doi.org/10.7256/2453-8922.2018.1.25833
Coverage:
Latitude: 70.384444 * Longitude: 68.317778
Minimum DEPTH, sediment/rock: 0.85 m * Maximum DEPTH, sediment/rock: 2.20 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Vasil'chuk, Yurij K | Geocode – from | |
2 | DEPTH, sediment/rock | Depth sed | m | Vasil'chuk, Yurij K | Geocode – to | |
3 | Sediment type | Sediment | Vasil'chuk, Yurij K | |||
4 | Layer description | Layer | Vasil'chuk, Yurij K |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
15 data points
Data
1 Depth sed [m] (from) | 2 Depth sed [m] (to) | 3 Sediment | 4 Layer |
---|---|---|---|
0.85 | 0.95 | Ice soil with fine-lenticular cryostructure (with ice schlieren 0.5-3 mm thick with the spacing between ice schlieren from 2 mm to 1 cm) | 1. (85-125 cm) a layer of ice soil passing along the whole section. The transition to the underlying patch is gradual in size and number of loam fragments, as well as in the type of the cryostructure. |
1.00 | 1.10 | Ice soil with reticulate cryostructure, with soil inclusions from 1 to 3 cm in size | 1. (85-125 cm) a layer of ice soil passing along the whole section. The transition to the underlying patch is gradual in size and number of loam fragments, as well as in the type of the cryostructure. |
1.10 | 1.25 | Clear ice with air bubbles and inclusions of prismatic loam fragments | 1. (85-125 cm) a layer of ice soil passing along the whole section. The transition to the underlying patch is gradual in size and number of loam fragments, as well as in the type of the cryostructure. |
1.30 | 1.50 | Fine-reticulate cryostructure, pieces of soil 1-3 mm in size | 2. (130-170 cm) ice soil, brown loam with ice |
1.50 | 1.70 | Coarse-reticulate cryostructure, clear ice with air bubbles | 2. (130-170 cm) ice soil, brown loam with ice |
1.70 | 1.80 | 3a. Sandy, loamy ice soil with reticulate cryostructure (mesh size from 2-3 mm to 2-3 cm) | |
1.80 | 1.90 | 3b. Layered sand with massive cryostructure and thin ice schlieren inclined at an angle of 45 degrees | |
1.90 | 2.00 | 3c. An inclined lens of sand in ice | |
2.10 | 2.20 | Clay-rich sand with mid-lenticular cryostructure | 3c. An inclined lens of sand in ice |