Schmieder, Frank (2004): Age model cyclostratigraphy of sediment core GeoB6425-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219530
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: -33.825200 * Longitude: -23.587300
Date/Time Start: 2000-03-02T08:02:00 * Date/Time End: 2000-03-02T08:02:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 10.61 m
Event(s):
GeoB6425-2 * Latitude: -33.825200 * Longitude: -23.587300 * Date/Time: 2000-03-02T08:02:00 * Elevation: -4352.0 m * Recovery: 10.89 m * Location: Central South Atlantic * Campaign: M46/4 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: geology and geophysics, CTD at 50 m
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:
58 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.00 |
| 0.23 | 22.00 |
| 0.72 | 66.00 |
| 0.85 | 84.00 |
| 0.92 | 88.00 |
| 1.03 | 100.00 |
| 1.11 | 110.00 |
| 1.23 | 122.00 |
| 1.54 | 156.00 |
| 1.91 | 182.00 |
| 2.20 | 214.00 |
| 2.28 | 226.00 |
| 2.45 | 240.00 |
| 2.85 | 274.00 |
| 2.99 | 288.00 |
| 3.09 | 298.00 |
| 3.49 | 328.00 |
| 3.58 | 344.00 |
| 3.81 | 360.00 |
| 4.28 | 408.00 |
| 4.47 | 432.00 |
| 4.61 | 444.00 |
| 4.90 | 470.00 |
| 5.07 | 484.00 |
| 5.13 | 490.00 |
| 5.35 | 502.00 |
| 5.59 | 514.00 |
| 5.72 | 526.00 |
| 5.75 | 527.62 |
| 6.06 | 527.62 |
| 6.09 | 546.00 |
| 6.18 | 562.00 |
| 6.30 | 576.00 |
| 6.33 | 586.00 |
| 6.37 | 596.00 |
| 6.46 | 604.00 |
| 6.56 | 616.00 |
| 6.83 | 646.00 |
| 7.18 | 676.00 |
| 7.42 | 690.00 |
| 7.60 | 720.00 |
| 7.73 | 732.00 |
| 7.93 | 756.00 |
| 8.29 | 784.00 |
| 8.46 | 802.00 |
| 8.61 | 820.00 |
| 8.73 | 832.00 |
| 8.93 | 860.00 |
| 9.20 | 890.00 |
| 9.41 | 908.00 |
| 9.56 | 924.00 |
| 9.89 | 954.00 |
| 9.96 | 966.00 |
| 10.06 | 976.00 |
| 10.13 | 986.00 |
| 10.27 | 998.00 |
| 10.41 | 1008.00 |
| 10.61 | 1022.00 |