Winn, Kyaw (2014): Susceptibility of sediment core GIK16128-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.831584
Always quote citation above when using data! You can download the citation in several formats below.
Published: 2014-04-08 • DOI registered: 2014-05-06
Related to:
Stoffers, Peter; Wright, I; Shipboard Scientific Party (1999): Cruise Report SONNE 135 - Havre Trough - Taupo Volcanic Zone: tectonic, magmatic and hydrothermal processes. Berichte-Reports, Institut für Geowissenschaften, Universität Kiel, 1, 250 pp, https://doi.org/10.2312/reports-ifg.1999.1
Project(s):
Coverage:
Latitude: -30.421250 * Longitude: -179.062433
Date/Time Start: 1998-09-25T09:23:00 * Date/Time End: 1998-09-25T09:23:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 0.830 m
Event(s):
Comment:
onboard measurements
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Susceptibility, magnetic | Mag sus | 10-6 cgs | Winn, Kyaw |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
84 data points
Data
1 Depth sed [m] | 2 Mag sus [10-6 cgs] |
---|---|
0.000 | 96 |
0.010 | 163 |
0.020 | 260 |
0.030 | 336 |
0.040 | 352 |
0.050 | 322 |
0.060 | 262 |
0.070 | 210 |
0.080 | 169 |
0.090 | 142 |
0.100 | 127 |
0.110 | 119 |
0.120 | 113 |
0.130 | 111 |
0.140 | 110 |
0.150 | 107 |
0.160 | 104 |
0.170 | 97 |
0.180 | 87 |
0.190 | 75 |
0.200 | 65 |
0.210 | 57 |
0.220 | 52 |
0.230 | 49 |
0.240 | 46 |
0.250 | 44 |
0.260 | 41 |
0.270 | 41 |
0.280 | 40 |
0.290 | 40 |
0.300 | 41 |
0.310 | 40 |
0.320 | 39 |
0.330 | 38 |
0.340 | 37 |
0.350 | 36 |
0.360 | 34 |
0.370 | 33 |
0.380 | 33 |
0.390 | 33 |
0.400 | 33 |
0.410 | 34 |
0.420 | 35 |
0.430 | 36 |
0.440 | 37 |
0.450 | 37 |
0.460 | 38 |
0.470 | 38 |
0.480 | 38 |
0.490 | 39 |
0.500 | 38 |
0.510 | 37 |
0.520 | 37 |
0.530 | 37 |
0.540 | 38 |
0.550 | 38 |
0.560 | 40 |
0.570 | 40 |
0.580 | 41 |
0.590 | 42 |
0.600 | 40 |
0.610 | 40 |
0.620 | 38 |
0.630 | 36 |
0.640 | 36 |
0.650 | 36 |
0.660 | 37 |
0.670 | 38 |
0.680 | 39 |
0.690 | 40 |
0.700 | 40 |
0.710 | 40 |
0.720 | 39 |
0.730 | 37 |
0.740 | 36 |
0.750 | 35 |
0.760 | 32 |
0.770 | 30 |
0.780 | 27 |
0.790 | 24 |
0.800 | 22 |
0.810 | 19 |
0.820 | 15 |
0.830 | 10 |