Thießen, Wolfgang; Bleil, Ulrich (2002): Age model of sediment core GeoB1413-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.66377
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: -15.680000 * Longitude: -9.455000
Date/Time Start: 1991-04-17T00:00:00 * Date/Time End: 1991-04-17T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 9.67 m
Event(s):
GeoB1413-4 * Latitude: -15.680000 * Longitude: -9.455000 * Date/Time: 1991-04-17T00:00:00 * Elevation: -3789.0 m * Recovery: 10.1 m * Location: West Angola Basin * Campaign: M16/1 * 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 GeoB1034-3 |
| 3 | Sedimentation rate | SR | cm/ka | Bleil, Ulrich | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
65 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 SR [cm/ka] |
|---|---|---|
| 0.00 | 0 | |
| 0.27 | 20 | 1.4 |
| 0.61 | 66 | 0.7 |
| 0.72 | 75 | 1.2 |
| 0.95 | 81 | 3.8 |
| 1.13 | 100 | 1.9 |
| 1.34 | 109 | 0.3 |
| 1.45 | 152 | 0.3 |
| 1.83 | 186 | 1.1 |
| 2.08 | 195 | 2.8 |
| 2.48 | 231 | 1.1 |
| 2.68 | 266 | 0.6 |
| 2.82 | 272 | 2.3 |
| 3.15 | 276 | 8.3 |
| 3.21 | 289 | 0.5 |
| 3.33 | 325 | 0.3 |
| 3.50 | 348 | 0.7 |
| 3.85 | 370 | 1.6 |
| 4.88 | 424 | 1.9 |
| 5.18 | 434 | 3.0 |
| 5.78 | 530 | 0.6 |
| 6.28 | 569 | 1.3 |
| 7.16 | 648 | 1.1 |
| 7.52 | 656 | 4.5 |
| 7.79 | 692 | 0.8 |
| 8.00 | 720 | 0.8 |
| 8.10 | 733 | 0.8 |
| 8.30 | 768 | 0.6 |
| 8.65 | 780 | 2.9 |
| 8.84 | 793 | 1.5 |
| 9.03 | 804 | 1.7 |
| 9.52 | 917 | 0.4 |
| 9.67 | 936 | 0.8 |