Sager, William W (2004): (Table T1) Paleomagnetic properties of igneous samples from DSDP Leg 17 sites [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.779531, In supplement to: Sager, WW (2004): Data report: Paleomagnetism of basaltic rocks cored from western Pacific DSDP and ODP boreholes. In: Sager, WW; Kanazawa, T; Escutia, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 191, 1-27, https://doi.org/10.2973/odp.proc.sr.191.003.2004
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 13.867233 * Median Longitude: -179.431100 * South-bound Latitude: 10.670000 * West-bound Longitude: 173.550000 * North-bound Latitude: 19.131700 * East-bound Longitude: -169.460000
Date/Time Start: 1971-05-08T00:00:00 * Date/Time End: 1971-05-19T00:00:00
Minimum DEPTH, sediment/rock: 190.27 m * Maximum DEPTH, sediment/rock: 338.03 m
Event(s):
17-169 * Latitude: 10.670000 * Longitude: 173.550000 * Date/Time: 1971-05-08T00:00:00 * Elevation: -5415.0 m * Penetration: 246.3 m * Recovery: 11.7 m * Location: North Pacific/BASIN * Campaign: Leg17 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 12 cores; 95.8 m cored; 0 m drilled; 12.2 % recovery
17-170 * Latitude: 11.800000 * Longitude: 177.616700 * Date/Time: 1971-05-12T00:00:00 * Elevation: -5792.0 m * Penetration: 196 m * Recovery: 31.6 m * Location: North Pacific/BASIN * Campaign: Leg17 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 8 cores; 72 m cored; 115 m drilled; 43.9 % recovery
17-171 * Latitude: 19.131700 * Longitude: -169.460000 * Date/Time: 1971-05-19T00:00:00 * Elevation: -2295.0 m * Penetration: 479 m * Recovery: 169.8 m * Location: North Pacific/GUYOT * Campaign: Leg17 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 27 cores; 296 m cored; 60 m drilled; 57.4 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Sager, William W | |||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 4 | NRM, Intensity | Inten (NRM) | mA/m | Sager, William W | ||
| 5 | ChRM, Inclination | Incl (ChRM) | deg | Sager, William W | Principal component analyses (PCA) | |
| 6 | Demag Type | Demag Type | Sager, William W | A = alternating field | ||
| 7 | Sample amount, subset | N subset | # | Sager, William W | number of measurements used for PCA | |
| 8 | Demagnetization level | Level | mT | Sager, William W | lower | |
| 9 | Demagnetization level | Level | mT | Sager, William W | upper | |
| 10 | Maximum angular deviation | MAD | deg | Sager, William W | ||
| 11 | Colatitude | Colat | deg | Sager, William W | ||
| 12 | Sample ID | Sample ID | Sager, William W | group number | ||
| 13 | Sample comment | Sample comment | Sager, William W |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
369 data points
Data
| 1 Event | 2 Sample label | 3 Depth sed [m] (mbsf) | 4 Inten (NRM) [mA/m] | 5 Incl (ChRM) [deg] | 6 Demag Type (A = alternating field) | 7 N subset [#] (number of measurements used f...) | 8 Level [mT] (lower) | 9 Level [mT] (upper) | 10 MAD [deg] | 11 Colat [deg] | 12 Sample ID (group number) | 13 Sample comment |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 17-169 | 17-169-6-1,27 | 190.27 | 700 | -52.9 | A | 4 | 15 | 40 | 4.5 | 123.5 | 17-169_1-sill | sill |
| 17-169 | 17-169-6-1,98 | 190.98 | 1400 | -46.7 | A | 4 | 15 | 40 | 4.4 | 118.0 | 17-169_1-sill | sill |
| 17-169 | 17-169-6-3,123 | 194.23 | 1400 | -56.2 | A | 3 | 35 | 45 | 5.1 | 126.7 | 17-169_1-sill | sill |
| 17-169 | 17-169-6-4,54 | 195.04 | 900 | -55.9 | A | 4 | 35 | 50 | 4.1 | 126.5 | 17-169_1-sill | sill |
| 17-169 | 17-169-6-4,99 | 195.49 | 2200 | -38.1 | A | 5 | 20 | 40 | 2.9 | 111.4 | 17-169_2-sill | sill |
| 17-169 | 17-169-6-5,49 | 196.49 | 1900 | -23.3 | A | 6 | 25 | 50 | 5.6 | 102.2 | 17-169_2-sill | sill |
| 17-169 | 17-169-11-1,82 | 233.82 | 5900 | 38.7 | A | 6 | 25 | 50 | 2.9 | 111.8 | 17-169_1-basalt | basalt flow; sample showing anomalous inclinations |
| 17-169 | 17-169-11-1,113 | 234.13 | 2300 | -40.7 | A | 5 | 15 | 35 | 3.9 | 113.3 | 17-169_1-basalt | basalt flow |
| 17-169 | 17-169-11-1,140 | 234.40 | 2800 | 17.1 | A | 4 | 10 | 25 | 1.4 | 98.7 | 17-169_1-basalt | basalt flow; sample showing anomalous inclinations; datum not used in average colatitude calculations |
| 17-169 | 17-169-12-1,2 | 238.02 | 2100 | -48.6 | A | 5 | 15 | 35 | 1.9 | 119.6 | 17-169_1-basalt | basalt flow |
| 17-169 | 17-169-12-1,36 | 238.36 | 1900 | -38.3 | A | 4 | 15 | 30 | 2.9 | 111.6 | 17-169_1-basalt | basalt flow |
| 17-169 | 17-169-12-1,133 | 239.33 | 5400 | -37.6 | A | 4 | 40 | 60 | 2.6 | 111.1 | 17-169_1-basalt | basalt flow |
| 17-169 | 17-169-12-2,42 | 239.92 | 7300 | -49.0 | A | 5 | 20 | 40 | 2.1 | 119.9 | 17-169_2-basalt | basalt flow |
| 17-169 | 17-169-12-2,49 | 239.99 | 4300 | -55.5 | A | 4 | 15 | 30 | 2.5 | 126.0 | 17-169_2-basalt | basalt flow |
| 17-169 | 17-169-12-2,77 | 240.27 | 5400 | -49.7 | A | 5 | 20 | 40 | 1.1 | 120.5 | 17-169_2-basalt | basalt flow |
| 17-169 | 17-169-12-2,110 | 240.60 | 3900 | -47.8 | A | 5 | 20 | 40 | 1.0 | 118.9 | 17-169_2-basalt | basalt flow |
| 17-170 | 17-170-16-1,84 | 192.84 | 1100 | -26.7 | A | 6 | 25 | 50 | 1.7 | 104.1 | 17-170_1 | |
| 17-170 | 17-170-16-1,93 | 192.93 | 2600 | 22.7 | A | 6 | 18 | 35 | 2.1 | 101.8 | 17-170_1 | sample showing anomalous inclinations |
| 17-170 | 17-170-16-1,107 | 193.07 | 4200 | 25.6 | A | 6 | 18 | 30 | 1.7 | 103.5 | 17-170_1 | sample showing anomalous inclinations |
| 17-170 | 17-170-16-2,25 | 193.75 | 3000 | -30.3 | A | 7 | 20 | 40 | 2.1 | 106.3 | 17-170_1 | |
| 17-170 | 17-170-16-2,56 | 194.06 | 3500 | -26.3 | A | 5 | 15 | 35 | 1.2 | 103.9 | 17-170_1 | |
| 17-170 | 17-170-16-2,85 | 194.35 | 2300 | -27.2 | A | 6 | 15 | 30 | 3.2 | 104.4 | 17-170_1 | |
| 17-170 | 17-170-16-2,122 | 194.72 | 1800 | 18.3 | A | 5 | 15 | 28 | 6.2 | 99.4 | 17-170_1 | sample showing anomalous inclinations |
| 17-171 | 17-171-27-1,46 | 334.46 | 4200 | -17.5 | A | 6 | 30 | 50 | 0.9 | 99.0 | 17-171_1 | |
| 17-171 | 17-171-27-1,68 | 334.68 | 5200 | -23.4 | A | 8 | 25 | 70 | 2.2 | 102.2 | 17-171_1 | |
| 17-171 | 17-171-27-1,109 | 335.09 | 4800 | -25.8 | A | 5 | 32 | 50 | 1.2 | 103.6 | 17-171_1 | |
| 17-171 | 17-171-27-1,144 | 335.44 | 3300 | -35.5 | A | 5 | 22 | 32 | 1.3 | 109.6 | 17-171_1 | |
| 17-171 | 17-171-27-2,12 | 335.62 | 3300 | -22.4 | A | 5 | 32 | 50 | 0.9 | 101.6 | 17-171_1 | |
| 17-171 | 17-171-27-2,68 | 336.18 | 6800 | -17.9 | A | 5 | 28 | 40 | 0.9 | 99.2 | 17-171_1 | |
| 17-171 | 17-171-27-2,115 | 336.65 | 7200 | -17.2 | A | 5 | 30 | 45 | 1.3 | 98.8 | 17-171_1 | |
| 17-171 | 17-171-27-2,138 | 336.88 | 6400 | -18.6 | A | 5 | 32 | 50 | 0.6 | 99.6 | 17-171_1 | |
| 17-171 | 17-171-27-3,34 | 337.34 | 4000 | -19.9 | A | 5 | 32 | 50 | 1.4 | 100.3 | 17-171_1 | |
| 17-171 | 17-171-27-3,43 | 337.43 | 2800 | -26.2 | A | 6 | 30 | 50 | 0.9 | 103.8 | 17-171_1 | |
| 17-171 | 17-171-27-3,72 | 337.72 | 3900 | -16.4 | A | 6 | 28 | 45 | 0.7 | 98.4 | 17-171_1 | |
| 17-171 | 17-171-27-3,103 | 338.03 | 4200 | -26.6 | A | 7 | 30 | 70 | 1.9 | 104.1 | 17-171_1 |