Bleil, Ulrich (1989): (Table 3) Magnetic reversal boundaries identified in ODP Hole 104-642C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.742898, In supplement to: Bleil, U (1989): Magnetostratigraphy of Neogene and Quaternary Sediment Series from the Norwegian Sea: Ocean Drilling Program, Leg 104. In: Eldholm, O.; Thiede, J.; Taylor, E.; et al. (eds.), Proceedings of the Ocean Drilling Program, 104 Scientific Results, Proceedings of the Ocean Drilling Program, 104, Ocean Drilling Program, 104, 829-902, https://doi.org/10.2973/odp.proc.sr.104.181.1989
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 67.220000 * Longitude: 2.930000
Date/Time Start: 1985-06-29T20:15:00 * Date/Time End: 1985-07-01T15:00:00
Minimum DEPTH, sediment/rock: 33.22 m * Maximum DEPTH, sediment/rock: 197.28 m
Event(s):
104-642C * Latitude: 67.220000 * Longitude: 2.930000 * Date/Time Start: 1985-06-29T20:15:00 * Date/Time End: 1985-07-01T15:00:00 * Elevation: -1292.0 m * Penetration: 199.6 m * Recovery: 194.93 m * Location: Norwegian Sea * Campaign: Leg104 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 199.6 m cored; 0 m drilled; 97.7 % recovery
Comment:
2.92 Ma = C2AN-1/C2AR-1 > hiatus > C2AN-2/C2AR-2 = 3.08 Ma. 6.70 Ma = C3BR/C4N-1 > 2 hiatuses and unresolved very predominantly normal polarity sequences in Cores 16 through 21 > C5AR-4/C5AN-5 = 12.83 Ma.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Bleil, Ulrich | DSDP/ODP/IODP sample designation | ||
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | Chronozone | Chronozone | Bleil, Ulrich | |||
4 | Age model | Age model | ka | Bleil, Ulrich | Age model, paleomagnetic | age model gives the ages of reversals boundary and are here linked to the lower subchron |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
110 data points
Data
1 Sample label | 2 Depth sed [m] | 3 Chronozone | 4 Age model [ka] |
---|---|---|---|
104-642C-5H-1,32 | 33.22 | C1N-1 | |
104-642C-5H-1,101 | 33.91 | C1R-1 | 730 |
104-642C-5H-5,33 | 39.23 | C1R-1 | |
104-642C-5H-5,101 | 39.91 | C1N-2 | 910 |
104-642C-6H-1,119 | 42.59 | C1N-2 | |
104-642C-6H-2,45 | 43.35 | C1R-2 | 980 |
104-642C-6H-6,119 | 50.09 | C1R-2 | |
104-642C-7H-1,110 | 52.00 | C2N | 1660 |
104-642C-7H-2,113 | 53.53 | C2N | |
104-642C-7H-3,41 | 54.31 | C2R | 1880 |
104-642C-7H-4,113 | 56.53 | C2R | |
104-642C-8H-1,41 | 57.51 | C2AN-1 | 2470 |
104-642C-9H-1,111 | 61.81 | C2AR-2 | |
104-642C-10H-1,41 | 63.91 | C2AN-3 | 3180 |
104-642C-10H-1,111 | 64.61 | C2AN-3 | |
104-642C-10H-6,43 | 71.43 | C2AR-3 | 3400 |
104-642C-11H-5,41 | 79.41 | C3R-2 | |
104-642C-11H-5,111 | 80.11 | C3N-3 | 4400 |
104-642C-12H-2,41 | 84.41 | C3N-4 | |
104-642C-12H-2,111 | 85.11 | C3R-4 | 4770 |
104-642C-13H-2,41 | 93.91 | C3R-4 | |
104-642C-13H-2,111 | 94.61 | C3AN-1 | 5350 |
104-642C-14H-2,111 | 104.11 | C3AN-1 | |
104-642C-14H-3,41 | 104.91 | C3AR-1 | 5530 |
104-642C-14H-4,41 | 106.41 | C3AR-1 | |
104-642C-14H-4,111 | 107.11 | C3AN-2 | 5680 |
104-642C-15H-3,40 | 114.40 | C3AN-2 | |
104-642C-15H-3,111 | 115.11 | C3AR-2 | 5890 |
104-642C-15H-5,109 | 118.09 | C3AR-2 | |
104-642C-16H-6,36 | 118.86 | C3BN | 6370 |
104-642C-15H-6,111 | 119.61 | C3BN | |
104-642C-15H-7,41 | 120.41 | C3BR | 6500 |
104-642C-22H-1,110 | 178.61 | C5AN-5 | |
104-642C-22H-2,41 | 179.41 | C5AR-5 | 13010 |
104-642C-22H-4,41 | 182.41 | C5AR-5 | |
104-642C-22H-4,111 | 183.11 | C5AN-6 | 13200 |
104-642C-23H-1,96 | 185.23 | C5AN-6 | |
104-642C-23H-2,29 | 186.09 | C5AR-6 | 13460 |
104-642C-23H-2,104 | 186.84 | C5AR-6 | |
104-642C-23H-3,29 | 187.59 | C5AN-7 | 13690 |
104-642C-23H-5,104 | 191.34 | C5AN-8 | |
104-642C-24H-1,52 | 192.92 | C5AR-8 | 14660 |
104-642C-24H-3,118 | 196.58 | C5BR-2 | |
104-642C-24H-4,38 | 197.28 | C5CN-1 | 16220 |