Denham, C R; Yeats, Robert S; Haq, Bilal U (2005): Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 63-469 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.261449
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Related to:
DSDP (1989): Data from the Deep Sea Drilling Project. Sediment, hard rock and reference files. National Geophysical Data Center, National Environmental Satellite, Data and Information Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1, CD-ROM
Wolfart, R; Shibata, Tsugio; Poore, Richard Z; Pisciotto, Kenneth A; Verma, Surendra P; Niem, Alan; Leinen, Margaret W; Grechin, V I; Douglas, A G; Denham, C R; Crouch, James; Bukry, David; Barron, John A; Yeats, Robert S; Haq, Bilal U (1981): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXIII, 967 pp, https://doi.org/10.2973/dsdp.proc.63.1981
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 32.616700 * Longitude: -120.548300
Date/Time Start: 1978-10-27T00:00:00 * Date/Time End: 1978-10-27T00:00:00
Minimum DEPTH, sediment/rock: 340.21 m * Maximum DEPTH, sediment/rock: 432.41 m
Event(s):
63-469 * Latitude: 32.616700 * Longitude: -120.548300 * Date/Time: 1978-10-27T00:00:00 * Elevation: -3790.0 m * Penetration: 453.5 m * Recovery: 170.2 m * Location: North Pacific/ESCARPMENT * Campaign: Leg63 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 49 cores; 436.5 m cored; 9.5 m drilled; 39 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Sample code/label | Sample label | Denham, C R | DSDP/ODP/IODP sample designation | ||
| 3 | Sample ID | Sample ID | Denham, C R | |||
| 4 | Lithology/composition/facies | Lithology | Denham, C R | |||
| 5 | NRM, Intensity | Inten (NRM) | mA/m | Denham, C R | reviewed and corrected (x 1000) by PANGAEA | |
| 6 | NRM, Inclination | Incl (NRM) | deg | Denham, C R | ||
| 7 | NRM, Declination | Decl (NRM) | deg | Denham, C R | ||
| 8 | ChRM, Inclination | Incl (ChRM) | deg | Denham, C R | ||
| 9 | Quality of orientation | Q orientation | Denham, C R | |||
| 10 | NRM, median destructive field of natural remanent magnetization, alternating field | MDF (NRM) | mT | Denham, C R | ||
| 11 | Magnetic susceptibility, volume | kappa | 10-6 SI | Denham, C R | Initial susceptibility [gauss/oersteds] transformed to 10**-6 SI | |
| 12 | Koenigsberger ratio | Q-ratio | A/m | Denham, C R | ||
| 13 | Sample method | Sample method | Denham, C R | Thermomagnetic curve | ||
| 14 | Curie temperature | Curie temp | °C | Denham, C R | ||
| 15 | Hysteresis, saturation magnetization, per unit volume | Ms | mA/m | Denham, C R | ||
| 16 | Hysteresis, saturation remanence, per unit volume | Msr | mA/m | Denham, C R | ||
| 17 | Coercive force | Bc | mT | Denham, C R | ||
| 18 | Coercivity of remanence | Bcr | mT | Denham, C R | Remanent coercive force | |
| 19 | Comment | Comment | Denham, C R |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
211 data points
Data
| 1 Depth sed [m] | 2 Sample label | 3 Sample ID | 4 Lithology | 5 Inten (NRM) [mA/m] | 6 Incl (NRM) [deg] | 7 Decl (NRM) [deg] | 8 Incl (ChRM) [deg] | 9 Q orientation | 10 MDF (NRM) [mT] | 11 kappa [10-6 SI] | 12 Q-ratio [A/m] | 13 Sample method | 14 Curie temp [°C] | 15 Ms [mA/m] | 16 Msr [mA/m] | 17 Bc [mT] | 18 Bcr [mT] | 19 Comment |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 340.21 | 63-469-37-1,20-22 | Tuff (sedimentary) | 61.70 | 128.90 | PUMICE | |||||||||||||
| 340.41 | 63-469-37-1,40-42 | Tuff (sedimentary) | 61.50 | 136.90 | PUMICE | |||||||||||||
| 369.53 | 63-469-40-1,102-104 | 1E | Igneous | 0.317 | 81.10 | 308.30 | ALT MOD,APHYRIC DOLERITE | |||||||||||
| 369.60 | 63-469-40-1,109-111 | 1E | Igneous | 0.392 | 18.0 | 4.1 | 201.06 | 0.054 | DIABASE,ALT MOD | |||||||||
| 374.64 | 63-469-41-3,13-15 | 1C | Igneous | 1.590 | 0.50 | 241.70 | ALT MOD,APHYRIC DOLERITE | |||||||||||
| 374.70 | 63-469-41-3,19-21 | 1C | Igneous | 2.080 | 0.90 | 245.20 | ALT MOD,APHYRIC DOLERITE | |||||||||||
| 375.13 | 63-469-41-3,62-64 | 1D | Igneous | 0.262 | 17.0 | 276.46 | 0.026 | DIABASE,ALT MOD | ||||||||||
| 381.23 | 63-469-42-3,22-24 | 1B | Igneous | 1.310 | -3.60 | 171.00 | ALT MOD,APHYRIC DOLERITE | |||||||||||
| 381.94 | 63-469-42-3,93-95 | 1B | Igneous | 0.562 | 9.30 | 169.60 | ALT MOD,APHYRIC DOLERITE | |||||||||||
| 383.17 | 63-469-42-4,66-68 | 1F | Igneous | 0.714 | -5.0 | 7.0 | 213.63 | 0.093 | Curie temperature is from the heating curve | 438 | 0.4800 | 0.04200 | 3.90 | 10.0 | DIABASE,ALT MOD | |||
| 383.17 | 63-469-42-4,66-68 | 1F | Igneous | Curie temperature is from the cooling curve | 495 | 0.6600 | 0.03800 | 3.10 | 10.6 | |||||||||
| 384.04 | 63-469-42-5,3-5 | 1A | Igneous | 0.904 | 6.20 | 335.00 | ALT MOD,APHYRIC DOLERITE | |||||||||||
| 384.54 | 63-469-42-5,53-55 | 1A | Igneous | 1.050 | 5.10 | 334.90 | ALT MOD,APHYRIC DOLERITE | |||||||||||
| 384.77 | 63-469-42-5,76-78 | 1B | Igneous | 0.615 | -3.0 | 7.1 | 213.63 | 0.080 | Curie temperature is from the heating curve | 404 | 0.4900 | 0.04600 | 3.80 | 8.4 | DIABASE,ALT MOD | |||
| 384.77 | 63-469-42-5,76-78 | 1B | Igneous | Curie temperature is from the cooling curve | 497 | 0.5700 | 0.05100 | 4.70 | 15.0 | |||||||||
| 385.72 | 63-469-42-6,21-23 | 1 | Igneous | 0.664 | unoriented | 9.2 | 289.03 | 0.064 | Curie temperature is from the cooling curve | 489 | 0.9300 | 0.06900 | 3.90 | 12.5 | DIABASE,ALT MOD | |||
| 385.72 | 63-469-42-6,21-23 | 1 | Igneous | Curie temperature is from the heating curve | 379 | 0.6800 | 0.08200 | 5.10 | 11.0 | |||||||||
| 399.14 | 63-469-44-3,13-15 | 1B | Igneous | 2.730 | -7.0 | 12.5 | 452.39 | 0.170 | APHYRIC BASALT,ALT MOD | |||||||||
| 407.65 | 63-469-45-2,114-116 | 4F | Igneous | 1.540 | 8.0 | 15.1 | 439.82 | 0.098 | Curie temperature is from the cooling curve | 489 | 0.8500 | 0.28000 | APHYRIC BASALT,ALT MOD | |||||
| 407.65 | 63-469-45-2,114-116 | 4F | Igneous | Curie temperature is from the heating curve | 309 | 1.0800 | 0.28000 | 10.60 | 14.7 | |||||||||
| 411.74 | 63-469-46-2,23-25 | 1D | Igneous | 0.680 | 25.0 | 263.89 | 0.072 | Curie temperature is from the heating curve | 317 | 0.5700 | 0.15000 | 12.00 | 18.7 | APHYRIC BASALT,ALT MOD | ||||
| 411.74 | 63-469-46-2,23-25 | 1D | Igneous | Curie temperature is from the cooling curve | 516 | 0.9900 | 0.16000 | 8.10 | 17.2 | |||||||||
| 432.41 | 63-469-49-1,40-42 | 6A | Igneous | 2.420 | unstable | 13.4 | 276.46 | 0.240 | APHYRIC BASALT,ALT MOD |