Foster, J H; Farrell, John W (2006): Age model of sediment core 85-573A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.356208
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: 0.498500 * Longitude: -133.309500
Date/Time Start: 1982-04-02T00:00:00 * Date/Time End: 1982-04-02T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 53.66 m
Event(s):
85-573A * Latitude: 0.498500 * Longitude: -133.309500 * Date/Time: 1982-04-02T00:00:00 * Elevation: -4301.0 m * Penetration: 57.7 m * Recovery: 53.4 m * Location: North Pacific/TROUGH * Campaign: Leg85 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 6 cores; 53.2 m cored; 0 m drilled; 100.4 % recovery
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:
47 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.0 |
| 6.24 | 305.0 |
| 6.61 | 344.0 |
| 7.01 | 380.0 |
| 7.71 | 441.0 |
| 8.41 | 475.0 |
| 8.97 | 522.0 |
| 9.61 | 588.0 |
| 10.01 | 641.0 |
| 10.01 | 1063.0 |
| 10.70 | 676.0 |
| 11.51 | 704.0 |
| 13.86 | 775.0 |
| 14.68 | 829.0 |
| 15.41 | 882.0 |
| 15.80 | 910.0 |
| 16.17 | 930.0 |
| 16.70 | 961.0 |
| 16.96 | 980.0 |
| 17.76 | 1050.0 |
| 18.30 | 1091.0 |
| 18.70 | 1123.0 |
| 19.11 | 1148.0 |
| 19.31 | 1172.0 |
| 19.80 | 1209.0 |
| 20.30 | 1243.0 |
| 21.01 | 1301.0 |
| 21.51 | 1353.0 |
| 22.20 | 1400.0 |
| 23.80 | 1549.0 |
| 24.70 | 1614.0 |
| 25.28 | 1660.0 |
| 26.93 | 1880.0 |
| 29.40 | 2056.0 |
| 33.31 | 2354.0 |
| 34.51 | 2441.0 |
| 34.89 | 2470.0 |
| 40.95 | 2920.0 |
| 41.20 | 2935.0 |
| 42.22 | 2990.0 |
| 42.75 | 3049.0 |
| 43.29 | 3080.0 |
| 44.30 | 3162.0 |
| 44.50 | 3180.0 |
| 47.80 | 3400.0 |
| 51.49 | 3632.0 |
| 53.66 | 3880.0 |