Abelmann, Andrea (1990): (Table 3) Definition and depth of stratigraphic datum points of ODP Hole 113-690B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.753359, 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
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -65.161000 * Longitude: 1.204900
Date/Time Start: 1987-01-20T03:15:00 * Date/Time End: 1987-01-21T07:00:00
Minimum DEPTH, sediment/rock: 31.72 m * Maximum DEPTH, sediment/rock: 53.25 m
Event(s):
113-690B * Latitude: -65.161000 * Longitude: 1.204900 * Date/Time Start: 1987-01-20T03:15:00 * Date/Time End: 1987-01-21T07:00:00 * Elevation: -2925.0 m * Penetration: 213.4 m * Recovery: 214.75 m * Location: South Atlantic Ocean * Campaign: Leg113 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 25 cores; 213.4 m cored; 0 m drilled; 100.6 % 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:
60 data points
Data
| 1 DL | 2 Age model [ka] | 3 Age min [ka] | 4 Depth sed [m] | 5 Chronozone |
|---|---|---|---|---|
| 1 | 11550 | 31.72 | Top C5AN-1 | |
| 2 | 11730 | 32.45 | Base C5AN-1 | |
| 3 | 11860 | 33.47 | Top C5AN-2 | |
| 4 | 12120 | 33.95 | Base C5AN-2 | |
| 5 | 12460 | 36.35 | Top C5AN-3 | |
| 6 | 12600 | 37.00 | Base C5AN-3 | |
| Hiatus N4A | 13800 | 12800 | 38.50 | |
| 7 | 14080 | 39.95 | Base C5AN-7 | |
| 8 | 14200 | 40.20 | Top C5AN-7 | |
| 9 | 14270 | 40.70 | Base C5AN-8 | |
| 10 | 14660 | 41.68 | Top C5BN-1 | |
| 11 | 14870 | 42.16 | Base C5BN-1 | |
| Hiatus N3 | ?17600 | ?15100 | 43.80 | |
| 12 | 17570 | 43.70 | Top C5DN-1 | |
| 13 | 17900 | 44.68 | Base C5DN-1 | |
| 14 | 18140 | 45.55 | Mid C5DN-1 | |
| Hiatus N2B | ?18700 | ?18500 | 47.10 | |
| Hiatus N2A | ?19600 | ?19000 | 48.70 | |
| Hiatus N1 | ?26600 | ?20000 | 51.20 | |
| 15 | 26860 | 53.25 | Top C8 |