Schmieder, Frank (2004): Age model cyclostratigraphy of sediment core GeoB6429-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219533
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: -31.950000 * Longitude: -24.248200
Date/Time Start: 2000-03-04T04:55:00 * Date/Time End: 2000-03-04T04:55:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.76 m
Event(s):
GeoB6429-2 * Latitude: -31.950000 * Longitude: -24.248200 * Date/Time: 2000-03-04T04:55:00 * Elevation: -4335.0 m * Recovery: 7.56 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:
102 data points
Data
1 Depth sed [m] | 2 Age model [ka] |
---|---|
0.00 | 0.00 |
0.09 | 18.00 |
0.15 | 44.00 |
0.22 | 66.00 |
0.29 | 102.00 |
0.39 | 156.00 |
0.41 | 170.00 |
0.47 | 182.00 |
0.54 | 226.00 |
0.55 | 240.00 |
0.60 | 274.00 |
0.64 | 328.00 |
0.72 | 358.00 |
0.83 | 408.00 |
0.89 | 470.00 |
0.97 | 486.00 |
1.08 | 526.00 |
1.18 | 546.00 |
1.27 | 574.00 |
1.39 | 616.00 |
1.47 | 676.00 |
1.55 | 692.00 |
1.65 | 720.00 |
1.71 | 732.00 |
1.74 | 756.00 |
1.87 | 784.00 |
1.88 | 904.00 |
1.95 | 924.00 |
2.00 | 954.00 |
2.02 | 966.00 |
2.19 | 998.00 |
2.23 | 1008.00 |
2.24 | 1022.00 |
2.33 | 1058.00 |
2.40 | 1080.00 |
2.48 | 1102.00 |
2.52 | 1108.00 |
2.61 | 1134.00 |
2.73 | 1164.00 |
2.82 | 1182.00 |
2.98 | 1214.00 |
3.06 | 1240.00 |
3.11 | 1260.00 |
3.15 | 1268.00 |
3.21 | 1280.00 |
3.32 | 1302.00 |
3.37 | 1314.00 |
3.46 | 1342.00 |
3.51 | 1360.00 |
3.57 | 1386.00 |
3.65 | 1398.00 |
3.74 | 1418.00 |
3.78 | 1442.00 |
3.81 | 1460.00 |
3.83 | 1490.00 |
3.85 | 1508.00 |
3.96 | 1524.00 |
4.05 | 1541.81 |
4.15 | 1570.79 |
4.24 | 1585.18 |
4.29 | 1627.64 |
4.38 | 1638.99 |
4.47 | 1672.73 |
4.58 | 1689.62 |
4.71 | 1708.12 |
4.83 | 1752.67 |
4.91 | 1766.67 |
5.02 | 1787.31 |
5.35 | 1917.50 |
5.40 | 1938.50 |
5.44 | 1958.50 |
5.49 | 1979.50 |
5.52 | 2002.50 |
5.56 | 2024.50 |
5.60 | 2043.50 |
5.64 | 2062.50 |
5.68 | 2081.50 |
5.71 | 2101.50 |
5.75 | 2125.50 |
5.79 | 2145.50 |
5.82 | 2165.50 |
5.86 | 2184.50 |
5.90 | 2206.50 |
5.93 | 2229.50 |
5.97 | 2248.50 |
6.01 | 2266.50 |
6.05 | 2285.50 |
6.08 | 2307.50 |
6.12 | 2328.50 |
6.16 | 2349.50 |
6.20 | 2368.50 |
6.24 | 2387.50 |
6.27 | 2407.50 |
6.32 | 2429.50 |
6.35 | 2449.50 |
6.40 | 2469.50 |
6.43 | 2489.50 |
6.48 | 2510.50 |
6.51 | 2531.50 |
6.55 | 2551.50 |
6.72 | 2652.50 |
6.76 | 2673.50 |