Foster, J H; Farrell, John W (2006): Age model of sediment core RC11-209 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.356218
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: 3.650000 * Longitude: -140.100000
Date/Time Start: 1967-09-07T00:00:00 * Date/Time End: 1967-09-07T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 14.11 m
Event(s):
RC11-209 * Latitude: 3.650000 * Longitude: -140.100000 * Date/Time: 1967-09-07T00:00:00 * Elevation: -4400.0 m * Recovery: 14.63 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:
63 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0 |
| 0.11 | 11 |
| 0.40 | 39 |
| 0.86 | 67 |
| 1.07 | 96 |
| 1.23 | 127 |
| 1.50 | 156 |
| 1.75 | 185 |
| 1.83 | 199 |
| 1.90 | 217 |
| 2.15 | 247 |
| 2.33 | 277 |
| 2.40 | 305 |
| 2.60 | 332 |
| 2.80 | 344 |
| 3.00 | 354 |
| 3.15 | 380 |
| 3.30 | 420 |
| 3.55 | 441 |
| 3.86 | 464 |
| 3.95 | 475 |
| 4.04 | 486 |
| 4.25 | 522 |
| 4.50 | 556 |
| 4.60 | 571 |
| 4.75 | 588 |
| 4.90 | 612 |
| 4.95 | 623 |
| 5.35 | 641 |
| 5.85 | 676 |
| 6.30 | 704 |
| 6.88 | 730 |
| 7.05 | 748 |
| 7.15 | 762 |
| 7.35 | 775 |
| 7.75 | 829 |
| 8.25 | 882 |
| 8.50 | 910 |
| 8.70 | 930 |
| 9.00 | 961 |
| 9.21 | 980 |
| 9.50 | 1050 |
| 9.70 | 1063 |
| 9.90 | 1091 |
| 10.10 | 1123 |
| 10.20 | 1148 |
| 10.40 | 1172 |
| 10.60 | 1209 |
| 10.75 | 1243 |
| 11.10 | 1301 |
| 11.35 | 1353 |
| 11.70 | 1400 |
| 11.95 | 1429 |
| 12.10 | 1458 |
| 12.30 | 1485 |
| 12.50 | 1506 |
| 12.80 | 1549 |
| 13.15 | 1614 |
| 13.41 | 1660 |
| 13.60 | 1725 |
| 13.85 | 1792 |
| 14.10 | 1868 |
| 14.11 | 1880 |