Foster, J H; Farrell, John W (2006): Age model of sediment core RC11-210 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.356221
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Foster, J H; Opdyke, Neil D (1970): Upper miocene to recent magnetic stratigraphy in deep-sea sediments. Journal of Geophysical Research: Solid Earth, 75(23), 4465-4473, https://doi.org/10.1029/JB075i023p04465
Project(s):
Coverage:
Latitude: 1.817000 * Longitude: -140.100000
Date/Time Start: 1967-09-08T00:00:00 * Date/Time End: 1967-09-08T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 13.55 m
Event(s):
RC11-210 * Latitude: 1.817000 * Longitude: -140.100000 * Date/Time: 1967-09-08T00:00:00 * Elevation: -4420.0 m * Recovery: 14.05 m * Campaign: RC11 (RC1112) * Basis: Robert Conrad * Method/Device: Piston corer (PC)
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 | Farrell, John W | compiled in Farrell & Prell, 1991 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
56 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0 |
| 0.14 | 12 |
| 0.67 | 39 |
| 1.22 | 67 |
| 1.27 | 69 |
| 1.35 | 77 |
| 1.45 | 89 |
| 1.51 | 96 |
| 1.55 | 100 |
| 1.67 | 113 |
| 1.83 | 127 |
| 2.28 | 156 |
| 2.72 | 185 |
| 2.88 | 199 |
| 3.04 | 217 |
| 3.35 | 243 |
| 3.40 | 247 |
| 3.68 | 266 |
| 3.84 | 277 |
| 4.08 | 303 |
| 4.12 | 305 |
| 4.40 | 322 |
| 4.60 | 332 |
| 4.96 | 344 |
| 5.24 | 354 |
| 5.60 | 380 |
| 5.75 | 411 |
| 5.88 | 420 |
| 6.40 | 441 |
| 6.96 | 464 |
| 7.14 | 475 |
| 7.26 | 486 |
| 7.60 | 522 |
| 8.16 | 556 |
| 8.35 | 571 |
| 8.50 | 586 |
| 8.52 | 588 |
| 8.84 | 612 |
| 9.04 | 623 |
| 9.44 | 641 |
| 10.10 | 671 |
| 10.20 | 676 |
| 10.30 | 682 |
| 10.72 | 704 |
| 11.24 | 724 |
| 11.36 | 728 |
| 11.42 | 730 |
| 11.50 | 733 |
| 11.63 | 748 |
| 11.76 | 762 |
| 11.92 | 775 |
| 12.32 | 829 |
| 12.75 | 882 |
| 13.15 | 910 |
| 13.44 | 961 |
| 13.55 | 980 |