Schmieder, Frank (2004): Age model cyclostratigraphy of sediment core GeoB1036-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219524
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: -21.173333 * Longitude: 3.328333
Date/Time Start: 1988-03-05T00:00:00 * Date/Time End: 1988-03-05T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 10.64 m
Event(s):
GeoB1036-1 * Latitude: -21.173333 * Longitude: 3.328333 * Date/Time: 1988-03-05T00:00:00 * Elevation: -5073.0 m * Penetration: 12 m * Location: Angola Basin * Campaign: M6/6 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: cc: Foram.-sand, weiß
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:
73 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.00 |
| 0.17 | 22.00 |
| 0.96 | 204.00 |
| 1.07 | 226.00 |
| 1.12 | 240.00 |
| 1.26 | 274.00 |
| 1.59 | 328.00 |
| 1.69 | 360.00 |
| 1.94 | 418.00 |
| 2.05 | 432.00 |
| 2.38 | 490.00 |
| 2.54 | 526.00 |
| 2.75 | 552.00 |
| 2.78 | 574.00 |
| 2.84 | 596.00 |
| 2.94 | 616.00 |
| 2.99 | 660.00 |
| 3.08 | 692.00 |
| 3.21 | 720.00 |
| 3.24 | 732.00 |
| 3.33 | 756.00 |
| 3.41 | 784.00 |
| 3.50 | 822.00 |
| 3.52 | 832.00 |
| 3.56 | 848.00 |
| 3.59 | 858.00 |
| 3.75 | 922.00 |
| 3.91 | 966.00 |
| 4.02 | 984.00 |
| 4.11 | 998.00 |
| 4.26 | 1008.00 |
| 4.31 | 1022.00 |
| 4.41 | 1058.00 |
| 4.53 | 1084.00 |
| 4.67 | 1098.00 |
| 4.77 | 1108.00 |
| 4.90 | 1134.00 |
| 5.16 | 1182.00 |
| 5.47 | 1214.00 |
| 5.59 | 1240.00 |
| 5.69 | 1268.00 |
| 5.82 | 1286.00 |
| 5.98 | 1302.00 |
| 6.09 | 1312.00 |
| 6.24 | 1342.00 |
| 6.38 | 1358.00 |
| 6.53 | 1386.00 |
| 6.79 | 1398.00 |
| 7.01 | 1420.00 |
| 7.09 | 1442.00 |
| 7.21 | 1462.00 |
| 7.31 | 1490.00 |
| 7.38 | 1508.00 |
| 7.49 | 1524.00 |
| 7.66 | 1541.50 |
| 7.73 | 1564.50 |
| 8.18 | 1585.50 |
| 8.31 | 1605.50 |
| 8.46 | 1626.50 |
| 8.60 | 1650.50 |
| 8.75 | 1671.50 |
| 8.96 | 1689.50 |
| 9.14 | 1708.50 |
| 9.26 | 1729.50 |
| 9.31 | 1752.00 |
| 9.52 | 1772.50 |
| 9.71 | 1793.50 |
| 9.86 | 1814.50 |
| 10.01 | 1836.50 |
| 10.19 | 1857.50 |
| 10.33 | 1877.50 |
| 10.47 | 1897.50 |
| 10.64 | 1918.50 |