Bro, Evgeny G (2007): Clay mineral composition of <0.001 mm size fraction of sedimentary rocks from Hole Vassdalensk-3 drilled in the West Svalbard [dataset]. All-Russian Research Institute for Geology and Mineral Resources of the World Ocean, St. Petersburg, PANGAEA, https://doi.org/10.1594/PANGAEA.615280, In: Bro, EG (1990): Processing results from parametric drill hole Vassdalenskaya-3, Svalbard Archipelago, north side of Van-Meyen Fjord (Report 6593, Leningrad) [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.690357
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 77.832100 * Longitude: 15.187500
Date/Time Start: 1988-02-28T00:00:00 * Date/Time End: 1989-09-01T00:00:00
Minimum DEPTH, sediment/rock: 837.30 m * Maximum DEPTH, sediment/rock: 2251.50 m
Event(s):
Vassdalensk-3 * Latitude: 77.832100 * Longitude: 15.187500 * Date/Time Start: 1988-02-28T00:00:00 * Date/Time End: 1989-09-01T00:00:00 * Elevation: 15.1 m * Penetration: 2481 m * Location: Svalbard * Campaign: VNIIO-1981S * 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 | Bro, Evgeny G | ||
3 | Depth, bottom/max | Depth bot | m | Bro, Evgeny G | ||
4 | Rock type | Rock | Bro, Evgeny G | |||
5 | Epoch | Epoch | Bro, Evgeny G | |||
6 | Hydromica | Hydromica | % | Bro, Evgeny G | X-ray diffraction, clay fraction | |
7 | Chlorite | Chl | % | Bro, Evgeny G | X-ray diffraction, clay fraction | |
8 | Kaolinite | Kln | % | Bro, Evgeny G | X-ray diffraction, clay fraction | |
9 | Montmorillonite | Mnt | % | Bro, Evgeny G | X-ray diffraction, clay fraction | |
10 | Mixed layer clay minerals | Mix layer | % | Bro, Evgeny G | X-ray diffraction, clay fraction | |
11 | Sum | Sum | % | Bro, Evgeny G | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
160 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Rock | 5 Epoch | 6 Hydromica [%] | 7 Chl [%] | 8 Kln [%] | 9 Mnt [%] | 10 Mix layer [%] | 11 Sum [%] |
---|---|---|---|---|---|---|---|---|---|---|
837.30 | 837.28 | 837.32 | siltstone | Paleocene | 70 | 30 | 0 | 0 | 0 | 100 |
839.00 | 838.98 | 839.02 | siltstone | Paleocene | 35 | 55 | 0 | 0 | 10 | 100 |
1420.20 | 1420.18 | 1420.22 | siltstone | Early Cretaceous, Barremian | 60 | 25 | 5 | 0 | 10 | 100 |
1421.10 | 1421.08 | 1421.12 | siltstone | Early Cretaceous, Barremian | 45 | 15 | 20 | 0 | 20 | 100 |
1423.30 | 1423.28 | 1423.32 | sandstone | Early Cretaceous, Barremian | 45 | 15 | 15 | 0 | 25 | 100 |
1426.40 | 1426.38 | 1426.42 | siltstone | Early Cretaceous, Barremian | 65 | 15 | 0 | 0 | 20 | 100 |
1429.00 | 1428.98 | 1429.02 | siltstone | Early Cretaceous, Barremian | 55 | 15 | 0 | 0 | 30 | 100 |
1429.00 | 1428.98 | 1429.02 | sandstone | Early Cretaceous, Barremian | 60 | 15 | 10 | 0 | 15 | 100 |
1487.80 | 1487.78 | 1487.82 | sandstone | Early Cretaceous, Barremian | 0 | 15 | 15 | 0 | 70 | 100 |
1773.00 | 1772.98 | 1773.02 | claystone | Late Jurassic - Early Cretaceous (Berriasian - Valanginian) | 80 | 5 | 5 | 0 | 10 | 100 |
1796.10 | 1796.08 | 1796.12 | claystone | Late Jurassic - Early Cretaceous (Berriasian - Valanginian) | 75 | 5 | 0 | 0 | 20 | 100 |
1823.50 | 1823.48 | 1823.52 | claystone | Late Jurassic - Early Cretaceous (Berriasian - Valanginian) | 85 | 5 | 0 | 0 | 10 | 100 |
1825.20 | 1825.18 | 1825.22 | claystone | Late Jurassic - Early Cretaceous (Berriasian - Valanginian) | 85 | 5 | 0 | 0 | 10 | 100 |
2007.40 | 2007.38 | 2007.42 | claystone | Early-Middle Jurassic | 80 | 0 | 0 | 0 | 20 | 100 |
2020.30 | 2020.28 | 2020.32 | claystone | Late Triassic, Norian | 70 | 5 | 0 | 0 | 25 | 100 |
2251.50 | 2251.48 | 2251.52 | sandstone | Late Triassic, Carnian | 35 | 55 | 0 | 0 | 10 | 100 |