Thießen, Wolfgang; Bleil, Ulrich (2002): Paleomagnetic analysis of sediment core GeoB1413-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.66737
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Schmieder, Frank (2004): Magnetic signals in Plio-Pleistocene sediments of the South Atlantic: Chronostratigraphic usability and paleooceanographic implications. In: Wefer, G; Mulitza, S & Ratmeyer, V (eds.), The South Atlantic in the Late Quaternary: Reconstruction of Material Budgets and Current Systems, Springer, Berlin, Heidelberg, New York, 261-277, https://doi.org/10.1007/978-3-642-18917-3_13
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: -15.680000 * Longitude: -9.455000
Date/Time Start: 1991-04-17T00:00:00 * Date/Time End: 1991-04-17T00:00:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 10.00 m
Event(s):
GeoB1413-4 * Latitude: -15.680000 * Longitude: -9.455000 * Date/Time: 1991-04-17T00:00:00 * Elevation: -3789.0 m * Recovery: 10.1 m * Location: West Angola Basin * Campaign: M16/1 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL)
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:
515 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] |
---|---|---|---|---|---|
0.05 | 1.560 | -26.6 | 360.0 | 1 | 19.00 |
0.10 | 2.870 | -9.0 | 356.0 | 1 | 21.10 |
0.20 | 2.170 | -45.6 | 350.4 | 1 | 28.50 |
0.30 | 3.020 | -18.9 | 9.5 | 1 | 44.30 |
0.40 | 1.680 | -29.3 | 18.5 | 1 | 37.40 |
0.50 | 1.240 | -28.2 | 14.7 | 1 | 35.60 |
0.60 | 1.000 | -23.9 | 12.7 | 1 | 36.40 |
0.70 | 1.860 | -27.5 | 16.2 | 1 | 43.00 |
0.80 | 1.290 | -32.7 | 5.3 | 1 | 23.10 |
0.90 | 1.210 | -27.8 | 355.0 | 1 | 18.90 |
1.00 | 0.580 | -33.0 | 334.8 | 1 | 14.50 |
1.10 | 0.770 | -26.3 | 315.3 | 1 | 20.80 |
1.20 | 0.860 | -23.8 | 23.4 | 1 | 20.70 |
1.30 | 0.560 | -42.5 | 5.6 | 1 | 25.80 |
1.40 | 2.010 | -33.0 | 349.3 | 1 | 43.60 |
1.50 | 1.700 | -34.0 | 339.8 | 1 | 46.40 |
1.60 | 1.210 | -35.8 | 342.6 | 1 | 39.80 |
1.70 | 1.490 | -34.1 | 344.6 | 1 | 35.80 |
1.80 | 1.020 | -32.3 | 348.8 | 1 | 32.20 |
1.90 | 0.340 | -30.2 | 18.2 | 1 | 11.40 |
2.00 | 0.660 | -30.1 | 22.9 | 1 | 22.20 |
2.10 | 0.950 | -31.6 | 1.9 | 1 | 25.70 |
2.20 | 0.530 | -37.3 | 355.9 | 1 | 17.60 |
2.30 | 0.940 | -34.9 | 351.1 | 1 | 27.50 |
2.40 | 0.530 | -37.4 | 0.2 | 1 | 21.70 |
2.50 | 0.780 | -28.2 | 6.6 | 1 | 34.50 |
2.60 | 0.930 | -30.1 | 355.5 | 1 | 33.90 |
2.70 | 3.130 | -38.1 | 355.2 | 1 | 53.90 |
2.80 | 1.490 | -37.4 | 357.0 | 1 | 43.20 |
2.90 | 0.470 | -20.4 | 353.1 | 1 | 21.30 |
3.00 | 0.390 | -21.4 | 7.1 | 1 | 21.70 |
3.10 | 0.550 | -30.5 | 17.0 | 1 | 22.50 |
3.20 | 0.560 | -13.2 | 6.0 | 1 | 22.30 |
3.30 | 0.610 | -23.8 | 4.2 | 1 | 14.40 |
3.40 | 0.600 | -28.3 | 14.4 | 1 | 16.80 |
3.50 | 1.950 | -28.5 | 1.2 | 1 | 30.20 |
3.60 | 1.640 | -28.6 | 356.8 | 1 | 40.40 |
3.70 | 1.400 | -33.3 | 358.8 | 1 | 39.50 |
3.80 | 2.030 | -30.6 | 358.2 | 1 | 45.60 |
3.90 | 3.680 | -31.2 | 1.6 | 1 | 46.80 |
4.00 | 2.300 | -30.1 | 358.0 | 1 | 32.50 |
4.10 | 1.190 | -39.7 | 351.6 | 1 | 33.80 |
4.20 | 0.480 | -27.6 | 347.3 | 1 | 27.00 |
4.30 | 0.410 | -26.8 | 345.6 | 1 | 19.90 |
4.40 | 0.250 | -24.0 | 28.3 | 1 | 27.60 |
4.50 | 1.030 | -31.2 | 355.5 | 1 | 35.40 |
4.60 | 1.020 | -34.8 | 354.2 | 1 | 33.20 |
4.70 | 0.830 | -30.1 | 356.1 | 1 | 33.30 |
4.80 | 1.330 | -17.9 | 351.9 | 1 | 47.00 |
4.90 | 3.200 | -36.6 | 6.2 | 1 | 38.20 |
5.00 | 1.200 | -35.9 | 355.9 | 1 | 33.80 |
5.10 | 1.580 | -39.3 | 7.7 | 1 | 37.30 |
5.20 | 2.280 | -32.6 | 20.7 | 1 | 34.40 |
5.30 | 1.680 | -26.8 | 16.7 | 1 | 27.70 |
5.40 | 1.280 | -26.6 | 16.8 | 1 | 24.40 |
5.50 | 1.310 | -26.3 | 6.3 | 1 | 23.00 |
5.60 | 0.490 | -29.0 | 5.0 | 1 | 17.60 |
5.70 | 0.410 | -29.8 | 353.2 | 1 | 11.60 |
5.80 | 0.360 | -31.7 | 345.9 | 1 | 8.00 |
5.90 | 0.450 | -25.0 | 348.5 | 1 | 8.90 |
6.00 | 0.380 | -27.6 | 343.3 | 1 | 6.70 |
6.10 | 0.380 | -24.8 | 344.5 | 1 | 6.60 |
6.20 | 0.770 | -34.2 | 358.5 | 1 | 8.00 |
6.30 | 1.180 | -26.9 | 4.6 | 1 | 9.20 |
6.40 | 0.540 | -26.1 | 7.3 | 1 | 35.90 |
6.50 | 0.580 | -27.8 | 358.3 | 1 | 9.10 |
6.60 | 0.890 | -29.0 | 6.2 | 1 | 16.70 |
6.70 | 0.590 | -24.7 | 358.7 | 1 | 9.20 |
6.80 | 1.130 | -38.6 | 359.7 | 1 | 10.00 |
6.90 | 0.900 | -17.0 | 7.0 | 1 | 8.70 |
7.00 | 0.880 | -30.6 | 345.2 | 1 | 8.30 |
7.10 | 2.010 | -30.5 | 353.0 | 1 | 20.60 |
7.20 | 3.030 | -29.9 | 358.5 | 1 | 32.00 |
7.30 | 2.110 | -33.0 | 1.1 | 1 | 26.40 |
7.40 | 3.490 | -29.1 | 356.1 | 1 | 33.90 |
7.50 | 5.230 | -28.5 | 359.0 | 1 | 35.90 |
7.60 | 1.140 | -27.8 | 357.5 | 1 | 19.00 |
7.70 | 1.740 | -30.8 | 6.0 | 1 | 25.40 |
7.80 | 0.530 | -41.0 | 353.6 | 1 | 6.50 |
7.90 | 0.920 | -32.8 | 0.9 | 1 | 6.60 |
8.00 | 1.640 | -31.3 | 6.7 | 1 | 15.70 |
8.10 | 0.800 | -29.2 | 6.9 | 1 | 8.00 |
8.20 | 1.180 | -35.5 | 2.6 | 1 | 12.30 |
8.30 | 4.140 | -31.1 | 359.8 | 1 | 41.10 |
8.40 | 1.960 | -31.0 | 357.3 | 1 | 29.70 |
8.50 | 0.740 | -29.0 | 354.9 | 1 | 12.00 |
8.60 | 0.140 | -38.9 | 1.6 | 1 | 6.20 |
8.63 | 0.310 | -22.8 | 26.9 | 1 | 9.20 |
8.66 | 0.300 | 39.2 | 180.2 | 2 | 15.90 |
8.70 | 0.810 | 27.8 | 177.4 | 2 | 7.30 |
8.80 | 2.340 | 25.4 | 186.0 | 2 | 10.60 |
8.90 | 2.150 | 31.7 | 180.7 | 2 | 18.80 |
9.00 | 0.770 | 27.7 | 182.5 | 2 | 10.10 |
9.10 | 0.840 | 35.3 | 186.2 | 2 | 8.90 |
9.20 | 1.130 | 26.5 | 178.5 | 2 | 8.10 |
9.30 | 1.210 | 26.2 | 177.1 | 2 | 5.70 |
9.40 | 1.790 | 27.3 | 166.8 | 2 | 5.80 |
9.48 | 2.280 | 27.1 | 192.0 | 2 | 8.10 |
9.60 | 2.520 | 26.6 | 190.9 | 2 | 37.50 |
9.70 | 0.750 | 27.4 | 189.9 | 2 | 8.90 |
9.80 | 1.510 | 19.5 | 164.8 | 2 | 19.80 |
9.90 | 6.960 | 29.2 | 179.7 | 2 | 42.80 |
10.00 | 0.770 | 27.5 | 175.6 | 2 | 5.70 |