Abelmann, Andrea (1990): (Table 2) Definition and depth of stratigraphic datum points of ODP Hole 113-689B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.753358, In supplement to: Abelmann, A (1990): Oligocene to middle Miocene radiolarian stratigraphy of southern high latitudes from Leg 113, sites 689 and 690, Maud Rise. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 675-708, https://doi.org/10.2973/odp.proc.sr.113.200.1990
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -64.517000 * Longitude: 3.099900
Date/Time Start: 1987-01-16T08:00:00 * Date/Time End: 1987-01-18T06:45:00
Minimum DEPTH, sediment/rock: 43.80 m * Maximum DEPTH, sediment/rock: 79.46 m
Event(s):
113-689B * Latitude: -64.517000 * Longitude: 3.099900 * Date/Time Start: 1987-01-16T08:00:00 * Date/Time End: 1987-01-18T06:45:00 * Elevation: -2091.0 m * Penetration: 297.3 m * Recovery: 229.45 m * Location: South Atlantic Ocean * Campaign: Leg113 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 33 cores; 297.3 m cored; 0 m drilled; 77.2 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Datum level | DL | Abelmann, Andrea | |||
| 2 | Age model | Age model | ka | Abelmann, Andrea | Age model, paleomag, Berggren et al (1985) | |
| 3 | Age, minimum/young | Age min | ka | Abelmann, Andrea | Age model, paleomag, Berggren et al (1985) | |
| 4 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 5 | Chronozone | Chronozone | Abelmann, Andrea |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
75 data points
Data
| 1 DL | 2 Age model [ka] | 3 Age min [ka] | 4 Depth sed [m] | 5 Chronozone |
|---|---|---|---|---|
| Hiatus N5 | 12300 | 11400 | 43.80 | |
| 1 | 12460 | 45.93 | Top C5AN-3 | |
| 2 | 12490 | 46.41 | Base C5AN-3 | |
| 3 | 12580 | 46.68 | Top C5AN-4 | |
| 4 | 12630 | 47.18 | Base C5AN-4 | |
| 5 | 12830 | 48.63 | Top C5AN-5 | |
| 6 | 13010 | 49.18 | Base C5AN-5 | |
| 7 | 13200 | 49.68 | Top C5AN-6 | |
| 8 | 13420 | 50.91 | Base C5AN-6 | |
| 9 | 14200 | 52.85 | Top C5AN-8 | |
| Hiatus N4 | 15000 | 14600 | 55.10 | |
| 10 | 15130 | 56.53 | Top C5BN-2 | |
| 11 | 15270 | 57.40 | Base C5BN-2 | |
| Hiatus N3 | ?17600 | ?15600 | 58.80 | |
| 12 | 17900 | 59.64 | Base C5DN-1 | |
| 13 | 18130 | 60.20 | Mid C5CDN-2 | |
| 14 | 18560 | 61.76 | Top C5EN | |
| Hiatus N2 | ?19400 | ?19100 | 64.76 | |
| Hiatus N1 | ?20000 | ?25600 | 66.86 | |
| 15 | 25970 | 68.00 | Base C7N-2 | |
| 16 | 26380 | 68.61 | Top C7AN | |
| 17 | 26560 | 68.88 | Base C7AN | |
| 18 | 26860 | 69.38 | Top C8N-1 | |
| 19 | 27740 | 75.98 | Base C8N-2 | |
| 20 | 28150 | 79.46 | Top C9N-1/2 |