Schmieder, Frank (2004): Age model cyclostratigraphy of sediment core GeoB6428-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219532
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: -32.510000 * Longitude: -24.248500
Date/Time Start: 2000-03-03T14:10:00 * Date/Time End: 2000-03-03T14:10:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 7.21 m
Event(s):
GeoB6428-1 * Latitude: -32.510000 * Longitude: -24.248500 * Date/Time: 2000-03-03T14:10:00 * Elevation: -4015.0 m * Recovery: 7.26 m * Location: Central South Atlantic * 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:
88 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.00 |
| 0.12 | 18.00 |
| 0.24 | 44.00 |
| 0.31 | 66.00 |
| 0.37 | 82.00 |
| 0.39 | 88.00 |
| 0.47 | 122.00 |
| 0.57 | 150.00 |
| 0.63 | 170.00 |
| 0.70 | 182.00 |
| 0.77 | 238.00 |
| 0.85 | 274.00 |
| 0.89 | 288.00 |
| 0.90 | 298.00 |
| 0.95 | 320.00 |
| 0.98 | 330.00 |
| 1.11 | 358.00 |
| 1.25 | 408.00 |
| 1.28 | 416.00 |
| 1.36 | 432.00 |
| 1.41 | 444.00 |
| 1.49 | 456.00 |
| 1.54 | 470.00 |
| 1.64 | 490.00 |
| 1.67 | 500.00 |
| 1.72 | 514.00 |
| 1.74 | 526.00 |
| 1.96 | 546.00 |
| 2.01 | 574.00 |
| 2.07 | 616.00 |
| 2.12 | 646.00 |
| 2.14 | 658.00 |
| 2.15 | 666.00 |
| 2.19 | 676.00 |
| 2.28 | 690.00 |
| 2.30 | 720.00 |
| 2.32 | 732.00 |
| 2.39 | 756.00 |
| 2.45 | 784.00 |
| 2.50 | 804.00 |
| 2.60 | 820.00 |
| 2.61 | 840.00 |
| 2.65 | 860.00 |
| 2.75 | 890.00 |
| 2.79 | 904.00 |
| 2.87 | 922.00 |
| 2.96 | 954.00 |
| 2.97 | 966.00 |
| 3.04 | 976.00 |
| 3.08 | 986.00 |
| 3.12 | 996.00 |
| 3.18 | 1008.00 |
| 3.25 | 1022.00 |
| 3.41 | 1058.00 |
| 3.53 | 1080.00 |
| 3.65 | 1100.00 |
| 3.71 | 1108.00 |
| 3.81 | 1134.00 |
| 4.07 | 1182.00 |
| 4.25 | 1212.00 |
| 4.34 | 1240.00 |
| 4.49 | 1268.00 |
| 4.58 | 1286.00 |
| 4.69 | 1302.00 |
| 4.75 | 1314.00 |
| 4.86 | 1342.00 |
| 4.95 | 1360.00 |
| 5.05 | 1386.00 |
| 5.12 | 1398.00 |
| 5.28 | 1420.00 |
| 5.39 | 1442.00 |
| 5.49 | 1462.00 |
| 5.59 | 1488.00 |
| 5.71 | 1508.00 |
| 5.80 | 1524.00 |
| 5.93 | 1542.50 |
| 6.05 | 1565.50 |
| 6.28 | 1585.50 |
| 6.36 | 1606.50 |
| 6.38 | 1626.50 |
| 6.49 | 1649.50 |
| 6.60 | 1672.50 |
| 6.70 | 1691.50 |
| 6.81 | 1708.50 |
| 6.91 | 1728.50 |
| 7.01 | 1751.50 |
| 7.10 | 1772.50 |
| 7.21 | 1792.50 |