Acton, Gary D; Galbrun, Bruno; King, John W (2000): (Table 16) ChRM inclinations and paleolatitudes of discrete samples from ODP Site 165-998 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.803354, In supplement to: Acton, GD et al. (2000): Paleolatitude of the Caribbean Plate since the Late Cretaceous. In: Leckie, RM; Sigurdsson, H; Acton, GD; Draper, G (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 165, 1-25, https://doi.org/10.2973/odp.proc.sr.165.001.2000
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 19.489600 * Longitude: -82.936100
Date/Time Start: 1995-12-28T21:15:00 * Date/Time End: 1996-02-01T12:15:00
Minimum DEPTH, sediment/rock: 6.61 m * Maximum DEPTH, sediment/rock: 902.22 m
Event(s):
165-998A * Latitude: 19.489600 * Longitude: -82.936100 * Date/Time Start: 1995-12-28T21:15:00 * Date/Time End: 1996-02-01T12:15:00 * Elevation: -3180.0 m * Penetration: 637.6 m * Recovery: 440.88 m * Location: Colombia Basin, Caribbean Sea * Campaign: Leg165 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 67 cores; 637.6 m cored; 0 m drilled; 69.1 % recovery
165-998B * Latitude: 19.489600 * Longitude: -82.936100 * Date/Time Start: 1996-02-01T12:15:00 * Date/Time End: 1996-01-08T15:00:00 * Elevation: -3180.0 m * Penetration: 904.8 m * Recovery: 287.88 m * Location: Colombia Basin, Caribbean Sea * Campaign: Leg165 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 37 cores; 346.5 m cored; 0 m drilled; 83.1 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Sample code/label | Sample label | Acton, Gary D | DSDP/ODP/IODP sample designation | ||
3 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
4 | ChRM, Inclination | Incl (ChRM) | deg | Acton, Gary D | Principal component analyses (PCA) | |
5 | Maximum angular deviation | MAD | deg | Acton, Gary D | MAD from the demagnetization data in the PCA | |
6 | Method comment | Method comm | Acton, Gary D | Principal component analysis (PCA): FRE = a lone fit throught the data only; ANC = a lone fit through the data, but anchored to the origin of the dematnetization plot; BRU = PCA results provided by Bruno Galburn | ||
7 | Paleolatitude | Pal-lat | Acton, Gary D |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
252 data points
Data
1 Event | 2 Sample label | 3 Depth sed [m] | 4 Incl (ChRM) [deg] | 5 MAD [deg] | 6 Method comm | 7 Pal-lat |
---|---|---|---|---|---|---|
165-998A | 165-998A-1H-5,61 | 6.61 | 37.7 | 2.88 | FRE | 21.13 |
165-998A | 165-998A-1H-6,61 | 8.11 | 48.7 | 5.44 | FRE | 29.65 |
165-998A | 165-998A-2H-2,61 | 10.91 | 55.4 | 7.41 | FRE | 35.93 |
165-998A | 165-998A-2H-4,11 | 13.41 | 38.1 | 9.28 | FRE | 21.41 |
165-998A | 165-998A-2H-4,61 | 13.91 | 46.7 | 9.32 | FRE | 27.95 |
165-998A | 165-998A-2H-5,61 | 15.41 | 37.7 | 6.98 | FRE | 21.13 |
165-998A | 165-998A-2H-6,61 | 16.91 | 28.9 | 7.71 | FRE | 15.43 |
165-998A | 165-998A-3H-5,61 | 24.91 | 30.1 | 9.37 | FRE | 16.16 |
165-998A | 165-998A-4H-5,61 | 34.41 | -21.9 | 4.43 | FRE | 11.36 |
165-998A | 165-998A-8H-3,61 | 69.41 | 21.9 | 1.78 | FRE | 11.36 |
165-998A | 165-998A-9H-2,62 | 77.42 | 38.8 | 3.52 | FRE | 21.90 |
165-998A | 165-998A-9H-5,61 | 81.91 | 22.0 | 6.54 | FRE | 11.42 |
165-998A | 165-998A-10H-4,61 | 89.91 | -24.4 | 9.87 | FRE | 12.78 |
165-998A | 165-998A-11H-3,50 | 97.80 | -16.9 | 4.25 | FRE | 8.64 |
165-998A | 165-998B-3R-4,80 | 582.00 | 36.2 | 1.92 | FRE | 20.10 |
165-998A | 165-998A-62X-2,146 | 582.86 | 42.6 | 9.50 | FRE | 24.69 |
165-998B | 165-998B-8R-3,83 | 628.60 | 28.1 | 2.59 | FRE | 14.95 |
165-998B | 165-998B-9R-4,68 | 639.70 | 28.6 | 6.81 | FRE | 15.25 |
165-998B | 165-998B-10R-3,90 | 647.80 | 37.4 | 4.44 | FRE | 20.92 |
165-998B | 165-998B-11R-2,109 | 656.00 | -17.2 | 0.40 | ANC | 8.80 |
165-998B | 165-998B-12R-3,126 | 667.10 | 24.3 | 8.90 | FRE | 12.72 |
165-998B | 165-998B-14R-4,14 | 687.50 | 25.3 | 1.94 | FRE | 13.30 |
165-998B | 165-998B-18R-4,147 | 726.50 | -6.1 | 9.28 | FRE | 3.06 |
165-998B | 165-998B-19R-2,105 | 733.10 | -11.4 | 8.66 | FRE | 5.76 |
165-998B | 165-998B-32R-1,124 | 848.33 | 3.3 | BRU | 1.65 | |
165-998B | 165-998B-32R-2,100 | 849.54 | -4.9 | BRU | 2.45 | |
165-998B | 165-998B-32R-3,110 | 851.14 | -2.2 | BRU | 1.10 | |
165-998B | 165-998B-32R-4,119 | 852.73 | -8.1 | BRU | 4.07 | |
165-998B | 165-998B-32R-5,109 | 854.13 | 14.4 | BRU | 7.32 | |
165-998B | 165-998B-32R-6,129 | 855.83 | -9.9 | BRU | 4.99 | |
165-998B | 165-998B-33R-1,90 | 857.59 | -12.9 | BRU | 6.53 | |
165-998B | 165-998B-33R-2,98 | 859.17 | 37.0 | BRU | 20.65 | |
165-998B | 165-998B-33R-3,99 | 860.68 | 18.9 | BRU | 9.71 | |
165-998B | 165-998B-33R-4,102 | 862.21 | 2.7 | BRU | 1.35 | |
165-998B | 165-998B-33R-5,114 | 863.83 | 18.4 | BRU | 9.44 | |
165-998B | 165-998B-33R-6,69 | 864.88 | -11.1 | BRU | 5.60 | |
165-998B | 165-998B-34R-1,115 | 867.44 | -10.4 | BRU | 5.24 | |
165-998B | 165-998B-34R-2,114 | 868.93 | -13.7 | BRU | 6.95 | |
165-998B | 165-998B-34R-3,114 | 870.43 | -6.2 | BRU | 3.11 | |
165-998B | 165-998B-34R-4,113 | 871.92 | -16.6 | BRU | 8.48 | |
165-998B | 165-998B-34R-5,110 | 873.39 | -16.0 | BRU | 8.16 | |
165-998B | 165-998B-34R-6,114 | 874.93 | -11.0 | BRU | 5.55 | |
165-998B | 165-998B-35R-1,36 | 876.25 | 25.0 | BRU | 13.12 | |
165-998B | 165-998B-35R-2,136 | 878.75 | 11.2 | BRU | 5.65 | |
165-998B | 165-998B-35R-3,142 | 880.31 | 20.5 | BRU | 10.59 | |
165-998B | 165-998B-35R-4,83 | 881.22 | 29.8 | BRU | 15.98 | |
165-998B | 165-998B-35R-5,125 | 883.14 | 34.5 | BRU | 18.96 | |
165-998B | 165-998B-35R-6,102 | 884.41 | 30.9 | BRU | 16.66 | |
165-998B | 165-998B-36R-1,114 | 886.63 | 26.0 | BRU | 13.71 | |
165-998B | 165-998B-36R-3,123 | 889.72 | 8.4 | BRU | 4.22 | |
165-998B | 165-998B-36R-4,114 | 891.13 | -15.4 | BRU | 7.84 | |
165-998B | 165-998B-36R-5,134 | 892.84 | -17.0 | BRU | 8.69 | |
165-998B | 165-998B-37R-1,24 | 895.33 | -15.0 | BRU | 7.63 | |
165-998B | 165-998B-37R-2,43 | 897.02 | -4.5 | BRU | 2.25 | |
165-998B | 165-998B-37R-3,104 | 899.13 | -6.6 | BRU | 3.31 | |
165-998B | 165-998B-37R-4,56 | 900.15 | 24.6 | BRU | 12.89 | |
165-998B | 165-998B-37R-5,113 | 902.22 | 44.7 | BRU | 26.33 |