Schmieder, Frank (2004): Paleomagnetic analysis of sediment core GeoB5142-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219502
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
Project(s):
Coverage:
Latitude: -19.090000 * Longitude: -17.145000
Date/Time Start: 1998-05-09T21:05:00 * Date/Time End: 1998-05-09T21:05:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 5.60 m
Event(s):
GeoB5142-1 * Latitude: -19.090000 * Longitude: -17.145000 * Date/Time: 1998-05-09T21:05:00 * Elevation: -3946.0 m * Recovery: 5.64 m * Location: Brazil Basin * Campaign: M41/3 (06MT41_3) * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 30 cm sediment recovered from the bomb and 25 cm sediment recovered from the core catcher, cc: nannofossil ooze, silty, very pale brown
Comment:
Demagnetization was performed at 5, 10, 15, 20, (25), 30, (35), 40, (45), 50, 65, 80, (95, 100, 110, 120) mT
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | ChRM, Inclination | Incl (ChRM) | deg | Schmieder, Frank | Single sample demagnetization | |
| 3 | ChRM, Declination | Decl (ChRM) | deg | Schmieder, Frank | Single sample demagnetization |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
224 data points
Data
| 1 Depth sed [m] | 2 Incl (ChRM) [deg] | 3 Decl (ChRM) [deg] |
|---|---|---|
| 0.05 | -17.5 | 16.1 |
| 0.10 | -28.8 | -4.7 |
| 0.15 | -33.6 | -8.3 |
| 0.20 | -30.8 | -13.7 |
| 0.25 | -29.7 | -4.9 |
| 0.30 | -27.3 | -7.0 |
| 0.35 | -28.4 | -9.3 |
| 0.40 | -24.3 | -6.7 |
| 0.45 | -32.3 | -0.7 |
| 0.50 | -31.1 | -4.7 |
| 0.55 | -33.3 | 3.4 |
| 0.60 | -36.3 | -14.4 |
| 0.65 | -32.7 | -24.6 |
| 0.70 | -36.2 | -12.7 |
| 0.74 | -32.3 | -5.6 |
| 0.80 | -28.5 | 12.0 |
| 0.85 | -24.2 | 9.6 |
| 0.90 | -23.2 | 23.7 |
| 0.95 | -23.7 | 11.2 |
| 1.00 | -24.1 | 11.5 |
| 1.05 | -27.6 | -2.4 |
| 1.10 | -33.0 | -7.9 |
| 1.15 | -36.8 | -3.9 |
| 1.20 | -25.4 | -1.5 |
| 1.25 | -25.3 | -7.5 |
| 1.30 | -33.2 | -10.5 |
| 1.35 | -26.1 | -3.8 |
| 1.40 | -34.3 | -6.2 |
| 1.45 | -43.8 | -11.0 |
| 1.50 | -34.7 | -0.4 |
| 1.55 | -23.8 | 5.2 |
| 1.60 | -32.3 | 8.3 |
| 1.65 | -25.2 | -1.8 |
| 1.70 | -23.6 | 3.2 |
| 1.74 | -31.7 | -2.0 |
| 1.81 | -30.9 | -6.2 |
| 1.86 | -27.2 | -2.3 |
| 1.91 | -26.9 | 6.3 |
| 1.96 | -30.7 | -5.6 |
| 2.01 | -29.2 | -5.3 |
| 2.06 | -35.9 | -3.3 |
| 2.11 | -42.5 | -19.5 |
| 2.16 | -39.1 | -17.5 |
| 2.21 | -40.3 | -11.2 |
| 2.26 | -37.2 | -15.7 |
| 2.31 | -36.9 | -10.2 |
| 2.36 | -36.0 | -8.5 |
| 2.41 | -30.6 | -8.7 |
| 2.46 | -34.2 | 1.7 |
| 2.51 | -33.0 | -8.3 |
| 2.56 | -34.1 | 0.1 |
| 2.61 | -31.8 | -10.3 |
| 2.66 | -32.2 | -9.1 |
| 2.71 | -34.5 | -4.6 |
| 2.75 | -40.4 | 0.4 |
| 2.80 | -33.7 | -10.7 |
| 2.85 | -30.4 | -4.8 |
| 2.90 | -43.9 | -2.7 |
| 2.95 | -40.8 | -11.5 |
| 3.00 | -41.6 | -6.7 |
| 3.05 | -38.2 | -0.4 |
| 3.10 | -34.6 | -4.5 |
| 3.15 | -32.0 | 2.4 |
| 3.20 | -38.0 | 0.4 |
| 3.25 | -34.0 | -6.3 |
| 3.30 | -30.7 | -1.8 |
| 3.35 | -29.1 | -6.1 |
| 3.40 | -34.8 | -5.8 |
| 3.45 | -33.2 | -4.9 |
| 3.50 | -35.4 | -2.3 |
| 3.55 | -39.4 | -2.5 |
| 3.60 | -39.1 | -6.9 |
| 3.65 | -40.4 | -9.8 |
| 3.70 | -35.5 | -7.8 |
| 3.75 | -36.6 | 6.0 |
| 3.80 | -34.7 | 10.8 |
| 3.85 | -34.5 | 9.2 |
| 3.90 | -35.4 | 10.8 |
| 3.95 | -34.2 | 19.7 |
| 4.00 | -35.1 | 12.2 |
| 4.05 | -34.2 | 13.0 |
| 4.10 | -28.0 | 16.0 |
| 4.15 | -32.0 | 11.0 |
| 4.20 | -35.8 | 12.1 |
| 4.25 | -35.4 | 12.5 |
| 4.30 | -30.2 | 14.5 |
| 4.35 | -33.7 | 8.0 |
| 4.40 | -26.4 | 14.9 |
| 4.45 | -38.8 | 12.0 |
| 4.50 | -36.5 | 10.2 |
| 4.55 | -39.0 | 6.3 |
| 4.60 | -40.7 | 13.0 |
| 4.65 | -30.2 | 14.8 |
| 4.70 | -26.9 | 13.3 |
| 4.75 | -17.8 | 31.2 |
| 4.80 | -31.5 | 9.0 |
| 4.85 | -38.4 | 1.8 |
| 4.90 | -33.9 | 7.4 |
| 4.95 | -34.3 | 3.7 |
| 5.00 | -36.0 | 0.3 |
| 5.05 | -40.0 | 1.6 |
| 5.10 | -38.1 | -0.3 |
| 5.15 | -41.9 | -6.3 |
| 5.20 | -37.9 | -2.4 |
| 5.25 | -36.7 | -5.8 |
| 5.30 | -36.9 | 5.5 |
| 5.35 | -47.9 | 20.6 |
| 5.40 | 35.8 | 163.5 |
| 5.45 | 56.2 | 172.1 |
| 5.50 | 44.9 | 142.8 |
| 5.55 | 50.6 | 170.6 |
| 5.60 | 42.0 | 166.5 |