Thießen, Wolfgang; Bleil, Ulrich (2002): Paleomagnetic analysis of sediment core GeoB1037-5 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.66720
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Thießen, Wolfgang (1993): Magnetische Eigenschaften von Sedimenten des östlichen Südatlantiks und ihre Paläozeanographische Relevanz. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 41, 170 pp, urn:nbn:de:gbv:46-ep000101793
Project(s):
Coverage:
Latitude: -13.153333 * Longitude: 0.145000
Date/Time Start: 1988-03-07T00:00:00 * Date/Time End: 1988-03-07T00:00:00
Minimum DEPTH, sediment/rock: 0.050 m * Maximum DEPTH, sediment/rock: 5.350 m
Event(s):
GeoB1037-5 * Latitude: -13.153333 * Longitude: 0.145000 * Date/Time: 1988-03-07T00:00:00 * Elevation: -5632.0 m * Penetration: 13 m * Location: Angola Basin * Campaign: M6/6 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: Tiefseeton, braun
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | NRM, Intensity | Inten (NRM) | mA/m | Bleil, Ulrich | Single sample demagnetization | |
3 | ChRM, Inclination | Incl (ChRM) | deg | Bleil, Ulrich | Single sample demagnetization | |
4 | ChRM, Declination | Decl (ChRM) | deg | Bleil, Ulrich | Single sample demagnetization | |
5 | ChRM, Polarity | Pol (ChRM) | Bleil, Ulrich | Single sample demagnetization | ||
6 | NRM, median destructive field, summarize of cumulative partial NRM, AF demag | MDF (spNRM) | mT | Bleil, Ulrich | Single sample demagnetization |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
237 data points
Data
1 Depth sed [m] | 2 Inten (NRM) [mA/m] | 3 Incl (ChRM) [deg] | 4 Decl (ChRM) [deg] | 5 Pol (ChRM) | 6 MDF (spNRM) [mT] |
---|---|---|---|---|---|
0.050 | 3.520 | -26.30 | 89.80 | 1 | 32.50 |
0.150 | 1.830 | -28.10 | 89.40 | 1 | 9.40 |
0.250 | 2.630 | -31.50 | 59.00 | 1 | 4.90 |
0.370 | 4.270 | -15.90 | 177.10 | 1 | 3.90 |
0.470 | 4.450 | 15.00 | 159.20 | 1 | 3.90 |
0.550 | 4.930 | -8.30 | 98.40 | 1 | 3.30 |
0.650 | 3.700 | 6.20 | 109.10 | 1 | 3.40 |
0.780 | 6.280 | -14.70 | 358.30 | 1 | 5.00 |
0.850 | 9.330 | -10.70 | 355.00 | 1 | 3.30 |
0.950 | 7.930 | -6.60 | 355.90 | 1 | 4.30 |
1.050 | 7.960 | -27.80 | 352.90 | 1 | 4.40 |
1.150 | 8.350 | -20.50 | 357.30 | 1 | 4.80 |
1.250 | 7.190 | -23.70 | 8.00 | 1 | 3.20 |
1.350 | 5.320 | 23.70 | 172.10 | 2 | 4.50 |
1.450 | 6.850 | 21.90 | 162.70 | 2 | 4.20 |
1.550 | 5.910 | 7.70 | 171.50 | 2 | 5.80 |
1.650 | 6.600 | 50.50 | 187.60 | 2 | 5.40 |
1.750 | 8.520 | 1.00 | 4.30 | 1 | 6.00 |
1.850 | 7.360 | -6.70 | 7.80 | 1 | 5.40 |
1.950 | 8.020 | -21.30 | 8.40 | 1 | 5.30 |
2.050 | 8.310 | -7.30 | 29.20 | 1 | 6.10 |
2.150 | 7.490 | 1.70 | 357.70 | 1 | 5.80 |
2.250 | 7.270 | -15.00 | 353.30 | 1 | 5.90 |
2.450 | 7.150 | 56.50 | 140.80 | 2 | 5.10 |
2.550 | 7.170 | 56.20 | 109.20 | 5.20 | |
2.650 | 6.930 | 21.30 | 160.50 | 2 | 5.70 |
2.750 | 6.000 | 22.90 | 169.50 | 2 | 5.80 |
2.850 | 7.880 | 5.60 | |||
2.950 | 6.270 | -8.90 | 101.70 | 2 | 5.10 |
3.050 | 5.150 | 16.80 | 156.90 | 2 | 6.10 |
3.150 | 8.320 | 5.50 | |||
3.250 | 5.970 | 8.40 | 323.10 | 1 | 6.50 |
3.360 | 5.870 | -4.40 | 336.00 | 1 | 7.40 |
3.470 | 4.760 | -22.40 | 17.50 | 1 | 5.20 |
3.560 | 5.070 | 3.40 | 147.50 | 9.00 | |
3.660 | 5.690 | -20.00 | 151.20 | 13.50 | |
3.760 | 5.780 | -61.90 | 84.00 | 3.90 | |
3.850 | 6.490 | 13.60 | 38.50 | 5.40 | |
3.960 | 4.270 | 8.80 | 106.80 | 5.40 | |
4.050 | 6.140 | 24.00 | 50.70 | 5.20 | |
4.150 | 5.950 | 4.40 | 103.50 | 5.60 | |
4.250 | 5.690 | 21.30 | 15.20 | 5.70 | |
4.350 | 4.190 | -9.70 | 128.90 | 6.30 | |
4.450 | 6.210 | -56.60 | 339.70 | 5.20 | |
4.550 | 5.640 | -9.70 | 195.10 | 6.70 | |
4.650 | 2.830 | -25.40 | 117.30 | 5.40 | |
4.750 | 6.120 | -34.00 | 128.60 | 5.60 | |
4.850 | 4.310 | 35.90 | 149.40 | 7.80 | |
4.950 | 6.150 | -19.90 | 60.70 | 5.80 | |
5.050 | 6.900 | -33.00 | 335.90 | 6.40 | |
5.150 | 7.790 | -4.80 | 84.30 | 5.80 | |
5.250 | 3.660 | 6.60 | |||
5.350 | 7.440 | 13.90 | 166.90 | 7.30 |