Schmieder, Frank (2004): Age model cyclostratigraphy of sediment core GeoB3724-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219527
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: -26.136667 * Longitude: 8.926667
Date/Time Start: 1996-02-15T00:00:00 * Date/Time End: 1996-02-15T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 11.17 m
Event(s):
GeoB3724-4 * Latitude: -26.136667 * Longitude: 8.926667 * Date/Time: 1996-02-15T00:00:00 * Elevation: -4763.0 m * Recovery: 11.41 m * Location: Northern Cape Basin * Campaign: M34/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: FGB
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:
36 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.00 |
| 3.35 | 478.00 |
| 3.64 | 536.00 |
| 4.23 | 574.00 |
| 4.36 | 616.00 |
| 5.11 | 688.00 |
| 6.22 | 784.00 |
| 6.55 | 806.00 |
| 6.68 | 822.00 |
| 6.87 | 846.00 |
| 7.03 | 860.00 |
| 7.15 | 890.00 |
| 7.42 | 904.00 |
| 7.53 | 922.00 |
| 7.70 | 954.00 |
| 8.42 | 1022.00 |
| 8.51 | 1058.00 |
| 8.67 | 1080.00 |
| 8.82 | 1102.00 |
| 8.89 | 1108.00 |
| 9.06 | 1134.00 |
| 9.41 | 1180.00 |
| 9.55 | 1212.00 |
| 9.74 | 1240.00 |
| 9.90 | 1268.00 |
| 10.03 | 1284.00 |
| 10.17 | 1302.00 |
| 10.25 | 1316.00 |
| 10.33 | 1342.00 |
| 10.48 | 1360.00 |
| 10.73 | 1386.00 |
| 10.89 | 1400.00 |
| 10.95 | 1420.00 |
| 11.07 | 1442.00 |
| 11.12 | 1462.00 |
| 11.17 | 1490.00 |