Ohneiser, Christian; Wilson, Gary S (2011): Paleomagnetic of sediment core DVDP-10 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.771464, In supplement to: Ohneiser, C; Wilson, GS (2012): Revised magnetostratigraphic chronologies for New Harbour drill cores, southern Victoria Land, Antarctica. Global and Planetary Change, 82-83, 12-24, https://doi.org/10.1016/j.gloplacha.2011.11.007
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Coverage:
Latitude: -77.578612 * Longitude: 163.511667
Date/Time Start: 1974-10-29T00:00:00 * Date/Time End: 1974-11-12T00:00:00
Minimum DEPTH, sediment/rock: 40.60 m * Maximum DEPTH, sediment/rock: 183.99 m
Event(s):
DVDP-10 * Latitude: -77.578612 * Longitude: 163.511667 * Date/Time Start: 1974-10-29T00:00:00 * Date/Time End: 1974-11-12T00:00:00 * Elevation: -2.8 m * Penetration: 185.9 m * Recovery: 206 m * Location: New Harbor * Campaign: DVDP * Basis: Sampling on land * 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 | Lithology/composition/facies | Lithology | Ohneiser, Christian | Visual description | ||
| 3 | Treatment | Treat | Ohneiser, Christian | |||
| 4 | Inclination | Incl | deg | Ohneiser, Christian | Principal component analyses (PCA) | |
| 5 | Declination | Decl | deg | Ohneiser, Christian | Principal component analyses (PCA) | |
| 6 | Maximum angular deviation | MAD | deg | Ohneiser, Christian | Principal component analyses (PCA) | |
| 7 | Behaviour | Behaviour | Ohneiser, Christian | see reference(s) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
198 data points
Data
| 1 Depth sed [m] | 2 Lithology | 3 Treat | 4 Incl [deg] | 5 Decl [deg] | 6 MAD [deg] | 7 Behaviour |
|---|---|---|---|---|---|---|
| 40.60 | silty clay | AF | -70.60 | 244.60 | 3.20 | B´´ |
| 41.39 | m sand with granules and silt | AF | -78.90 | 189.70 | 3.40 | B´ |
| 55.09 | clay with silt | AF | 69.30 | 319.20 | 2.60 | A´ |
| 55.09 | clay with silt | Thermal | 69.60 | 329.40 | 10.40 | C |
| 55.47 | mud with pebbles | AF | 64.90 | 222.60 | 5.30 | B´ |
| 58.88 | sandy mud with pebbles | AF | -64.00 | 198.10 | 4.70 | B´ |
| 59.40 | mud with clast (5mm) | AF | -86.90 | 61.80 | 5.70 | C |
| 90.59 | silt clay with clasts | AF | 70.81 | 66.99 | 6.32 | B´´ |
| 96.03 | clay with abundent vc sand and granules | AF | -75.82 | 54.20 | 9.86 | B´´ |
| 106.00 | mud with clast (10 mm) | Thermal | -49.60 | 188.20 | 9.40 | B´ |
| 112.14 | muddy silt | AF | 78.70 | 330.00 | 8.30 | B |
| 113.59 | siltstone with 8 mm clast | AF | -82.90 | 54.10 | 5.90 | B´ |
| 114.56 | siltstone with granules | AF | 47.10 | 325.20 | 6.30 | B´ |
| 116.04 | silty mud with clasts | AF | 80.11 | 355.89 | 10.91 | C |
| 118.98 | muddy siltstone with disperesed clasts | AF | -82.70 | 347.10 | 5.50 | B |
| 119.78 | silty clay with granules and pebbles | AF | -76.60 | 283.10 | 2.30 | A |
| 121.03 | mud with granules | Thermal | -82.30 | 341.90 | 5.80 | B |
| 121.03 | mud with granules | AF | -79.50 | 337.50 | 4.10 | B´ |
| 122.43 | mud with pebbles | AF | -77.60 | 236.00 | 4.60 | B´ |
| 124.06 | mud with granules | AF | -80.81 | 148.79 | 15.97 | C |
| 141.27 | clay with pebbles (7mm) | AF | 81.10 | 146.20 | 13.00 | C |
| 142.43 | silty m/c sandstone | AF | -81.30 | 128.46 | 4.20 | B´ |
| 152.35 | clay with rare granules | Thermal | 66.10 | 105.60 | 3.40 | B |
| 158.58 | siltstone | AF | -76.50 | 176.80 | 0.50 | A |
| 159.46 | mudstone | AF | -74.20 | 170.90 | 2.70 | A´ |
| 170.68 | mud with disperesed clasts | AF | 81.10 | 130.70 | 4.10 | B |
| 172.44 | mudstone with granules | Thermal | 51.90 | 274.80 | 6.80 | B´ |
| 172.44 | mudstone with granules | AF | 79.60 | 265.70 | 2.40 | A |
| 179.82 | claystone and m sandstone bed | AF | 80.50 | 60.00 | 0.90 | A |
| 180.20 | mud | AF | 70.18 | 93.49 | 8.50 | B´´ |
| 180.20 | mud | Thermal | 81.62 | 108.21 | 8.58 | B´´ |
| 181.82 | bedded clay and silt and m/f sand | AF | 75.74 | 200.25 | 2.14 | A´ |
| 183.99 | siltstone | AF | -83.80 | 169.10 | 5.50 | B |