von Dobeneck, Tilo; Schmieder, Frank (2004): Inclination of sediment core GeoB1729-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.227260
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Schmieder, Frank (1999): Magnetic cyclostratigraphy of South Altantic sediments. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 135, 82 pp, urn:nbn:de:gbv:46-ep000102535
von Dobeneck, Tilo; Schmieder, Frank (1999): Using rock magnetic proxy records for orbital and extended time series analyses into the super- and sub-Milankovitch bands. In: Fischer, G & Wefer, G (eds.), Use of Proxies in Paleoceanography - Examples from the South Atlantic, Springer, Berlin, Heidelberg, 601-633
Project(s):
Coverage:
Latitude: -28.893333 * Longitude: 1.001667
Date/Time Start: 1992-01-22T00:00:00 * Date/Time End: 1992-01-22T00:00:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 7.40 m
Event(s):
GeoB1729-3 * Latitude: -28.893333 * Longitude: 1.001667 * Date/Time: 1992-01-22T00:00:00 * Elevation: -4401.0 m * Recovery: 7.45 m * Location: Namibia continental slope * Campaign: M20/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: CC: Karbonatschl., fest, Foram.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Inclination | Incl | deg | Schmieder, Frank | Single sample demagnetization |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
75 data points
Data
| 1 Depth sed [m] | 2 Incl [deg] |
|---|---|
| 0.05 | 12.7 |
| 0.10 | 2.5 |
| 0.20 | -50.0 |
| 0.30 | -53.5 |
| 0.40 | -55.0 |
| 0.50 | -54.3 |
| 0.60 | -47.6 |
| 0.70 | -48.1 |
| 0.80 | -53.1 |
| 0.90 | -49.8 |
| 1.00 | -52.4 |
| 1.10 | -49.0 |
| 1.20 | -56.3 |
| 1.30 | -52.8 |
| 1.40 | -55.1 |
| 1.50 | -59.3 |
| 1.60 | -55.0 |
| 1.70 | -59.1 |
| 1.80 | -58.6 |
| 1.90 | -56.4 |
| 2.00 | -50.8 |
| 2.10 | -52.5 |
| 2.20 | -55.4 |
| 2.30 | -56.1 |
| 2.40 | -56.2 |
| 2.50 | -57.5 |
| 2.60 | -53.8 |
| 2.70 | -49.4 |
| 2.80 | -53.5 |
| 2.90 | -57.4 |
| 3.00 | -47.7 |
| 3.10 | -53.5 |
| 3.20 | -54.8 |
| 3.30 | -54.0 |
| 3.40 | -43.4 |
| 3.50 | -58.5 |
| 3.60 | -58.1 |
| 3.70 | -62.6 |
| 3.80 | -60.0 |
| 3.90 | -55.6 |
| 4.00 | -50.0 |
| 4.10 | -55.1 |
| 4.20 | -47.2 |
| 4.30 | -49.5 |
| 4.40 | -56.5 |
| 4.50 | -58.2 |
| 4.60 | -55.3 |
| 4.70 | -61.4 |
| 4.80 | 40.0 |
| 4.90 | 52.1 |
| 5.00 | 41.1 |
| 5.10 | 50.3 |
| 5.20 | 55.2 |
| 5.30 | 51.4 |
| 5.40 | 49.7 |
| 5.50 | 42.9 |
| 5.60 | 49.0 |
| 5.70 | 31.2 |
| 5.80 | 55.4 |
| 5.90 | 57.3 |
| 6.00 | -55.5 |
| 6.10 | -47.6 |
| 6.20 | -52.7 |
| 6.30 | -53.4 |
| 6.40 | -51.8 |
| 6.50 | -57.6 |
| 6.60 | -74.6 |
| 6.70 | 24.9 |
| 6.80 | 42.3 |
| 6.90 | 50.1 |
| 7.00 | 41.9 |
| 7.10 | 41.7 |
| 7.20 | 53.0 |
| 7.30 | 48.5 |
| 7.40 | 48.1 |