Schmieder, Frank (2004): Age model cyclostratigraphy of sediment core GeoB6426-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219531
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: -33.499200 * Longitude: -24.024200
Date/Time Start: 2000-03-02T15:41:00 * Date/Time End: 2000-03-02T15:41:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 13.20 m
Event(s):
GeoB6426-1 * Latitude: -33.499200 * Longitude: -24.024200 * Date/Time: 2000-03-02T15:41:00 * Elevation: -4385.0 m * Recovery: 13.41 m * Campaign: M46/4 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: geology and geophysics
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:
57 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.00 |
| 0.19 | 22.00 |
| 0.75 | 66.00 |
| 0.91 | 82.00 |
| 1.26 | 122.00 |
| 1.58 | 158.00 |
| 1.95 | 182.00 |
| 2.21 | 214.00 |
| 2.32 | 226.00 |
| 2.44 | 240.00 |
| 2.86 | 274.00 |
| 3.05 | 288.00 |
| 3.58 | 328.00 |
| 3.80 | 358.00 |
| 4.27 | 412.00 |
| 4.45 | 432.00 |
| 4.57 | 442.00 |
| 4.86 | 470.00 |
| 5.05 | 490.00 |
| 5.29 | 502.00 |
| 5.47 | 512.00 |
| 5.60 | 524.00 |
| 5.84 | 546.00 |
| 6.00 | 560.00 |
| 6.07 | 576.00 |
| 6.31 | 616.00 |
| 6.62 | 646.00 |
| 6.89 | 676.00 |
| 7.19 | 692.00 |
| 7.34 | 718.00 |
| 7.49 | 734.00 |
| 7.71 | 756.00 |
| 8.06 | 784.00 |
| 8.22 | 800.00 |
| 8.42 | 820.00 |
| 8.77 | 860.00 |
| 9.00 | 890.00 |
| 9.18 | 904.00 |
| 9.37 | 922.00 |
| 9.69 | 954.00 |
| 9.80 | 966.00 |
| 9.93 | 986.00 |
| 10.03 | 998.00 |
| 10.18 | 1008.00 |
| 10.43 | 1026.00 |
| 10.72 | 1058.00 |
| 10.96 | 1082.00 |
| 11.15 | 1100.00 |
| 11.25 | 1108.00 |
| 11.46 | 1132.00 |
| 11.92 | 1182.00 |
| 12.37 | 1212.00 |
| 12.58 | 1240.00 |
| 12.76 | 1268.00 |
| 12.91 | 1284.00 |
| 13.07 | 1302.00 |
| 13.20 | 1314.00 |