Wessels, Martin; Grobe, Hannes; Villinger, Heinrich (1989): Sound velocity of sediment core PS1397-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.50926, In supplement to: Wessels, Martin (1989): Sedimentationsprozesse an der Filchner Schelfeiskante, Antarktis. Diploma Thesis, Institut und Museum für Geologie und Paläontologie der Georg-August-Universität zu Göttingen (in Zusammenarbeit mit dem Alfred-Wegener-Institut), 126 pp, hdl:10013/epic.30827.d001
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Project(s):
Coverage:
Latitude: -76.876667 * Longitude: -50.025000
Date/Time Start: 1986-01-14T13:03:00 * Date/Time End: 1986-01-14T13:03:00
Minimum DEPTH, sediment/rock: 0.06 m * Maximum DEPTH, sediment/rock: 0.32 m
Event(s):
PS1397-1 (PS08/380) * Latitude: -76.876667 * Longitude: -50.025000 * Date/Time: 1986-01-14T13:03:00 * Elevation: -270.0 m * Penetration: 0.41 m * Recovery: 0.41 m * Location: Filchner Shelf * Campaign: ANT-IV/3 (PS08) * Basis: Polarstern * Method/Device: Giant box corer (GKG)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Velocity, compressional wave | Vp | m/s | Villinger, Heinrich | ||
3 | Velocity, compressional, amplitude | Vp-a | Villinger, Heinrich |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
54 data points
Data
1 Depth sed [m] | 2 Vp [m/s] | 3 Vp-a |
---|---|---|
0.06 | 1185.0 | 0.001 |
0.07 | 1179.0 | 0.003 |
0.08 | 1166.0 | 0.017 |
0.09 | 1176.0 | 0.039 |
0.10 | 1220.0 | 0.050 |
0.11 | 1274.0 | 0.066 |
0.13 | 1287.0 | 0.072 |
0.14 | 1215.0 | 0.056 |
0.15 | 1273.0 | 0.038 |
0.16 | 1203.0 | 0.045 |
0.17 | 1225.0 | 0.036 |
0.18 | 1254.0 | 0.014 |
0.19 | 1341.0 | 0.006 |
0.20 | 1354.0 | 0.004 |
0.21 | 1384.0 | 0.004 |
0.22 | 1389.0 | 0.002 |
0.23 | 1429.0 | 0.002 |
0.24 | 1435.0 | 0.009 |
0.25 | 1425.0 | 0.029 |
0.26 | 1434.0 | 0.049 |
0.27 | 1544.0 | 0.045 |
0.28 | 1558.0 | 0.036 |
0.29 | 1520.0 | 0.034 |
0.29 | 1479.0 | 0.023 |
0.30 | 1558.0 | 0.015 |
0.31 | 1531.0 | 0.013 |
0.32 | 1550.0 | 0.011 |