Wolf, Thomas C W; Wolf-Welling, Thomas C W (2001): Age model of ODP Hole 104-643A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.58164
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Baumann, Karl-Heinz (1990): Veränderlichkeit der Coccolithophoridenflora des Europäischen Nordmeeres im Jungquartär. Berichte aus dem Sonderforschungsbereich 313, Christian-Albrechts-Universität, Kiel, 22, 146 pp, https://doi.org/10.2312/reports-sfb313.1990.22
Goll, Robert M (1989): A synthesis of Norwegian Sea biostratigraphies: ODP Leg 104 on the Vøring Plateau. In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 777-826, https://doi.org/10.2973/odp.proc.sr.104.203.1989
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 67.715000 * Longitude: 1.033300
Date/Time Start: 1985-08-03T06:07:00 * Date/Time End: 1985-08-08T01:45:00
Minimum DEPTH, sediment/rock: 2.31 m * Maximum DEPTH, sediment/rock: 400.40 m
Event(s):
104-643A * Latitude: 67.715000 * Longitude: 1.033300 * Date/Time Start: 1985-08-03T06:07:00 * Date/Time End: 1985-08-08T01:45:00 * Elevation: -2780.0 m * Penetration: 565.2 m * Recovery: 458.29 m * Location: Norwegian Sea * Campaign: Leg104 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 62 cores; 565.2 m cored; 0 m drilled; 81.1 % 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 | Wolf-Welling, Thomas C W | Age model, composite | |
3 | Age, comment | Comm | Wolf-Welling, Thomas C W |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
148 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
---|---|---|
2.31 | 79 | Isotopenstratigraphie |
2.51 | 85 | BAUMANN (1990) |
2.71 | 99 | Isotopenstratigraphie |
2.80 | 105 | BAUMANN (1990) |
3.04 | 123 | Isotopenstratigraphie |
3.19 | 127 | BAUMANN (1990) |
6.30 | 175 | Isotopenstratigraphie |
6.80 | 187 | BAUMANN (1990) |
7.20 | 215 | Isotopenstratigraphie |
7.73 | 240 | Isotopenstratigraphie |
8.60 | 280 | BAUMANN (1990) |
9.30 | 291 | BAUMANN (1990) |
9.72 | 299 | BAUMANN (1990) |
10.08 | 310 | Isotopenstratigraphie |
12.82 | 405 | Isotopenstratigraphie |
13.28 | 423 | BAUMANN (1990) |
14.90 | 502 | BAUMANN (1990) |
16.00 | 560 | BAUMANN (1990) |
16.90 | 574 | BAUMANN (1990) |
17.12 | 600 | BAUMANN (1990) |
24.30 | 700 | GOLL (1989) |
33.80 | 1000 | GOLL (1989) |
43.30 | 1300 | GOLL (1989) |
45.50 | 1600 | GOLL (1989) |
45.50 | 1900 | GOLL (1989) |
51.50 | 2600 | GOLL (1989) |
51.50 | 3200 | GOLL (1989) |
52.80 | 3300 | GOLL (1989) |
62.30 | 4200 | GOLL (1989) |
62.30 | 5600 | GOLL (1989) |
69.30 | 6000 | GOLL (1989) |
69.30 | 6900 | GOLL (1989) |
81.30 | 7700 | GOLL (1989) |
90.80 | 8200 | GOLL (1989) |
100.30 | 8800 | GOLL (1989) |
100.30 | 13700 | GOLL (1989) |
102.90 | 13900 | GOLL (1989) |
102.90 | 14100 | GOLL (1989) |
109.80 | 14300 | GOLL (1989) |
114.20 | 14500 | GOLL (1989) |
114.20 | 14800 | GOLL (1989) |
119.50 | 14900 | GOLL (1989) |
128.80 | 15200 | GOLL (1989) |
134.40 | 15300 | GOLL (1989) |
134.40 | 15600 | GOLL (1989) |
138.30 | 15700 | GOLL (1989) |
147.80 | 16000 | GOLL (1989) |
152.30 | 16200 | GOLL (1989) |
166.80 | 16400 | GOLL (1989) |
176.30 | 16700 | GOLL (1989) |
185.80 | 16900 | GOLL (1989) |
195.30 | 17100 | GOLL (1989) |
205.10 | 17300 | GOLL (1989) |
214.90 | 17600 | GOLL (1989) |
224.70 | 17800 | GOLL (1989) |
234.50 | 18000 | GOLL (1989) |
244.30 | 18200 | GOLL (1989) |
254.10 | 18500 | GOLL (1989) |
263.90 | 18700 | GOLL (1989) |
273.80 | 19000 | GOLL (1989) |
273.80 | 19700 | GOLL (1989) |
283.50 | 20000 | GOLL (1989) |
293.30 | 20300 | GOLL (1989) |
303.10 | 20500 | GOLL (1989) |
312.90 | 20800 | GOLL (1989) |
322.70 | 21200 | GOLL (1989) |
332.50 | 21400 | GOLL (1989) |
342.30 | 21700 | GOLL (1989) |
352.10 | 22000 | GOLL (1989) |
361.80 | 22300 | GOLL (1989) |
371.40 | 22600 | GOLL (1989) |
381.10 | 22900 | GOLL (1989) |
390.70 | 23200 | GOLL (1989) |
400.40 | 23500 | GOLL (1989) |