Thießen, Wolfgang; Bleil, Ulrich (2002): Age model of sediment core GeoB1209-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.66376
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Thießen, Wolfgang (1993): Magnetische Eigenschaften von Sedimenten des östlichen Südatlantiks und ihre Paläozeanographische Relevanz. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 41, 170 pp, urn:nbn:de:gbv:46-ep000101793
Project(s):
Coverage:
Latitude: -24.508333 * Longitude: 7.293333
Date/Time Start: 1990-03-20T00:00:00 * Date/Time End: 1990-03-20T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 7.25 m
Event(s):
GeoB1209-2 * Latitude: -24.508333 * Longitude: 7.293333 * Date/Time: 1990-03-20T00:00:00 * Elevation: -3357.0 m * Recovery: 10.05 m * Location: Cape Basin * Campaign: M12/1 * 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 | Bleil, Ulrich | Age model, lithological correlation | Correlation of magnet. suscept. with GeoB1214-1 and GeoB1034-3 and paleomagnetic |
3 | Sedimentation rate | SR | cm/ka | Bleil, Ulrich | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
83 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 SR [cm/ka] |
---|---|---|
0.00 | 0 | |
0.12 | 6 | 2.0 |
0.31 | 41 | 0.5 |
0.38 | 53 | 0.6 |
0.45 | 88 | 0.2 |
0.61 | 95 | 2.3 |
0.87 | 126 | 0.8 |
1.04 | 154 | 0.6 |
1.13 | 173 | 0.5 |
1.19 | 189 | 0.4 |
1.23 | 192 | 1.3 |
1.30 | 209 | 0.4 |
1.33 | 221 | 0.3 |
1.40 | 237 | 0.4 |
1.42 | 241 | 0.5 |
1.48 | 255 | 0.4 |
1.51 | 271 | 0.2 |
1.67 | 309 | 0.4 |
1.93 | 351 | 0.6 |
2.00 | 360 | 0.8 |
2.15 | 410 | 0.3 |
2.28 | 427 | 0.8 |
2.89 | 556 | 0.5 |
2.90 | 569 | 0.1 |
3.21 | 613 | 0.7 |
3.27 | 648 | 0.2 |
3.36 | 651 | 3.0 |
3.41 | 656 | 1.0 |
3.56 | 692 | 0.4 |
3.90 | 720 | 1.2 |
4.04 | 768 | 0.3 |
4.23 | 780 | 1.6 |
4.63 | 851 | 0.6 |
5.18 | 917 | 0.8 |
5.60 | 968 | 0.8 |
5.68 | 990 | 0.4 |
6.13 | 1070 | 0.6 |
6.26 | 1078 | 1.6 |
6.40 | 1100 | 0.6 |
6.59 | 1126 | 0.7 |
6.78 | 1150 | 0.8 |
7.25 | 1190 | 1.1 |