Schmieder, Frank (2004): Age model cyclostratigraphy of sediment core GeoB5142-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219529
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: 0.00 m * Maximum DEPTH, sediment/rock: 5.48 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
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Age model | Age model | ka | Schmieder, Frank | Age model, paleomagnetic |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
30 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.00 |
| 0.03 | 52.00 |
| 0.17 | 66.00 |
| 0.61 | 158.00 |
| 0.92 | 182.00 |
| 1.00 | 194.00 |
| 1.12 | 226.00 |
| 1.25 | 238.00 |
| 1.45 | 274.00 |
| 1.57 | 288.00 |
| 1.79 | 320.00 |
| 1.98 | 330.00 |
| 2.18 | 360.00 |
| 2.55 | 408.00 |
| 2.69 | 432.00 |
| 2.77 | 444.00 |
| 2.96 | 470.00 |
| 3.12 | 484.00 |
| 3.31 | 502.00 |
| 3.74 | 546.00 |
| 4.10 | 576.00 |
| 4.28 | 616.00 |
| 4.51 | 674.00 |
| 4.65 | 690.00 |
| 4.74 | 720.00 |
| 4.84 | 732.00 |
| 5.05 | 756.00 |
| 5.27 | 784.00 |
| 5.38 | 802.00 |
| 5.48 | 822.00 |