Schmieder, Frank (2004): Age model cyclostratigraphy of sediment core GeoB1413-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219526
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: -15.680000 * Longitude: -9.455000
Date/Time Start: 1991-04-17T00:00:00 * Date/Time End: 1991-04-17T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 9.90 m
Event(s):
GeoB1413-4 * Latitude: -15.680000 * Longitude: -9.455000 * Date/Time: 1991-04-17T00:00:00 * Elevation: -3789.0 m * Recovery: 10.1 m * Location: West Angola Basin * Campaign: M16/1 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL)
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:
45 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.00 |
| 0.27 | 22.00 |
| 0.74 | 66.00 |
| 0.85 | 82.00 |
| 0.98 | 98.00 |
| 1.07 | 110.00 |
| 1.13 | 122.00 |
| 1.44 | 158.00 |
| 1.83 | 182.00 |
| 1.99 | 196.00 |
| 2.10 | 204.00 |
| 2.18 | 214.00 |
| 2.33 | 226.00 |
| 2.44 | 240.00 |
| 2.69 | 274.00 |
| 2.89 | 288.00 |
| 3.38 | 328.00 |
| 3.52 | 360.00 |
| 3.88 | 396.00 |
| 4.06 | 408.00 |
| 4.89 | 432.00 |
| 5.02 | 444.00 |
| 5.26 | 470.00 |
| 5.52 | 484.00 |
| 5.54 | 490.00 |
| 5.59 | 500.00 |
| 5.69 | 512.00 |
| 5.86 | 526.00 |
| 6.33 | 546.00 |
| 6.57 | 562.00 |
| 6.66 | 576.00 |
| 6.86 | 616.00 |
| 7.15 | 658.00 |
| 7.48 | 676.00 |
| 7.78 | 690.00 |
| 7.94 | 720.00 |
| 8.08 | 732.00 |
| 8.29 | 756.00 |
| 8.56 | 784.00 |
| 8.83 | 804.00 |
| 9.04 | 820.00 |
| 9.31 | 860.00 |
| 9.55 | 890.00 |
| 9.71 | 904.00 |
| 9.90 | 924.00 |