Gruetzner, Jens; Higgins, Sean M (2010): (Table 1) Initial depth tie points between ODP Site 162-983 and IODP Site 306-U1314 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.770378, In supplement to: Gruetzner, J; Higgins, SM (2010): Threshold behavior of millennial scale variability in deep water hydrography inferred from a 1.1 Ma long record of sediment provenance at the southern Gardar Drift. Paleoceanography, 25, PA4204, https://doi.org/10.1029/2009PA001873
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Project(s):
Coverage:
Latitude: 56.364000 * Longitude: -27.888000
Date/Time Start: 2005-04-07T00:00:00 * Date/Time End: 2005-04-10T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 168.90 m
Event(s):
306-U1314 * Latitude: 56.364000 * Longitude: -27.888000 * Date/Time Start: 2005-04-07T00:00:00 * Date/Time End: 2005-04-10T00:00:00 * Elevation: -2800.0 m * Recovery: 765.63 m * Location: North Atlantic * Campaign: Exp306 (North Atlantic Climate 2) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
Comment:
Sediment depth is given in mcd.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Depth, reference | Depth ref | m | Gruetzner, Jens | Intercore correlation | Site 162-983 depth in mcd |
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
33 data points
Data
| 1 Depth ref [m] | 2 Depth sed [m] |
|---|---|
| 0.00 | 0.00 |
| 1.88 | 2.08 |
| 3.08 | 2.61 |
| 4.75 | 3.46 |
| 6.86 | 4.42 |
| 9.26 | 6.60 |
| 11.66 | 8.60 |
| 15.36 | 12.04 |
| 22.36 | 15.24 |
| 27.16 | 19.58 |
| 42.77 | 29.38 |
| 50.57 | 35.52 |
| 53.97 | 37.20 |
| 56.07 | 38.44 |
| 62.57 | 42.98 |
| 63.87 | 43.74 |
| 66.07 | 45.26 |
| 69.70 | 47.45 |
| 80.07 | 53.10 |
| 90.66 | 59.10 |
| 103.92 | 69.25 |
| 117.24 | 77.70 |
| 127.50 | 82.95 |
| 131.83 | 84.50 |
| 173.88 | 106.78 |
| 186.35 | 115.40 |
| 209.42 | 131.35 |
| 223.83 | 140.70 |
| 234.49 | 144.05 |
| 246.99 | 150.20 |
| 262.04 | 158.15 |
| 276.10 | 166.10 |
| 281.80 | 168.90 |