Schmieder, Frank (2004): Age model cyclostratigraphy of sediment core GeoB1307-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219525
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: -33.601667 * Longitude: -27.665000
Date/Time Start: 1991-01-30T00:00:00 * Date/Time End: 1991-01-30T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.15 m
Event(s):
GeoB1307-1 * Latitude: -33.601667 * Longitude: -27.665000 * Date/Time: 1991-01-30T00:00:00 * Elevation: -4017.0 m * Recovery: 6.77 m * Location: Hunter Channel * Campaign: M15/2 (06MT15_2) * 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:
59 data points
Data
1 Depth sed [m] | 2 Age model [ka] |
---|---|
0.00 | 0.00 |
0.13 | 18.00 |
0.24 | 66.00 |
0.32 | 100.00 |
0.54 | 170.00 |
0.70 | 182.00 |
0.75 | 238.00 |
0.94 | 274.00 |
1.20 | 328.00 |
1.21 | 860.00 |
1.31 | 890.00 |
1.44 | 904.00 |
1.56 | 924.00 |
1.67 | 954.00 |
1.70 | 966.00 |
1.75 | 974.00 |
1.78 | 984.00 |
1.80 | 998.00 |
1.82 | 1008.00 |
1.84 | 1022.00 |
1.92 | 1058.00 |
2.00 | 1078.00 |
2.06 | 1108.00 |
2.11 | 1134.00 |
2.21 | 1182.00 |
2.32 | 1214.00 |
2.38 | 1240.00 |
2.46 | 1268.00 |
2.69 | 1342.00 |
2.81 | 1460.00 |
3.09 | 1541.81 |
3.17 | 1570.79 |
3.41 | 1668.98 |
3.65 | 1711.84 |
3.76 | 1766.67 |
3.91 | 1787.31 |
4.07 | 1917.37 |
4.20 | 1950.00 |
4.34 | 2169.51 |
4.38 | 2209.52 |
4.42 | 2249.28 |
4.48 | 2304.64 |
4.51 | 2327.81 |
4.53 | 2345.09 |
4.57 | 2394.17 |
4.62 | 2447.04 |
4.66 | 2486.94 |
4.72 | 2517.18 |
4.78 | 2550.78 |
4.80 | 2581.00 |
4.86 | 2652.99 |
4.98 | 2720.21 |
5.01 | 2749.01 |
5.05 | 2777.82 |
5.30 | 3040.00 |
5.50 | 3110.00 |
5.60 | 3220.00 |
5.78 | 3330.00 |
6.15 | 3580.00 |