Kluger, Max Oke; Moon, Vicki G; Kreiter, Stefan; Lowe, David J; Churchman, G J; Hepp, Daniel A; Seibel, David; Jorat, Ehsan M; Mörz, Tobias (2017): (Figure 2c) Halloysite bulk concentration of drill core Omok-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.871098, In supplement to: Kluger, MO et al. (2017): A new attraction-detachment model for explaining flow sliding in clay-rich tephras. Geology, 45(2), 131-134, https://doi.org/10.1130/G38560.1
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Project(s):
Coverage:
Latitude: -37.635000 * Longitude: 176.045000
Minimum DEPTH, sediment/rock: 2.80 m * Maximum DEPTH, sediment/rock: 38.40 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Kluger, Max Oke | Geocode | |
| 2 | Halloysite | Halloysite | % | Kluger, Max Oke | wt. % |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
55 data points
Data
| 1 Depth sed [m] | 2 Halloysite [%] |
|---|---|
| 2.80 | 3.4207 |
| 5.00 | 36.4800 |
| 8.50 | 15.9407 |
| 11.50 | 10.0787 |
| 14.00 | 12.1500 |
| 16.20 | 21.3381 |
| 17.20 | 13.8592 |
| 17.40 | 13.4261 |
| 17.60 | 10.8379 |
| 18.00 | 10.2249 |
| 18.20 | 28.7790 |
| 18.40 | 30.8374 |
| 18.50 | 18.9364 |
| 18.60 | 20.1703 |
| 18.80 | 23.7609 |
| 19.00 | 32.5829 |
| 19.20 | 23.3469 |
| 19.40 | 31.7280 |
| 19.50 | 28.1134 |
| 19.60 | 23.8849 |
| 20.20 | 29.8301 |
| 20.50 | 31.8217 |
| 21.00 | 39.1420 |
| 21.40 | 41.9771 |
| 21.90 | 35.7669 |
| 22.50 | 27.9099 |
| 22.60 | 38.6224 |
| 23.10 | 34.8265 |
| 23.30 | 37.2220 |
| 23.50 | 39.6211 |
| 23.70 | 38.7091 |
| 23.90 | 36.9723 |
| 24.00 | 40.7249 |
| 24.10 | 37.6039 |
| 24.20 | 32.9091 |
| 24.40 | 34.2602 |
| 24.60 | 36.0236 |
| 25.15 | 39.3495 |
| 25.95 | 42.5825 |
| 26.12 | 9.5190 |
| 26.20 | 12.0500 |
| 26.40 | 8.9220 |
| 26.60 | 13.8700 |
| 26.80 | 13.4501 |
| 26.95 | 9.0300 |
| 27.00 | 11.2400 |
| 27.40 | 14.5944 |
| 27.60 | 11.5800 |
| 27.80 | 11.5800 |
| 28.00 | 8.7100 |
| 28.60 | 7.6200 |
| 29.20 | 4.3700 |
| 32.00 | 6.2900 |
| 34.90 | 6.0468 |
| 38.40 | 0.2932 |