Smith, Guy M; Bougault, Henri; Cande, Steven C (2005): Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 82-558. PANGAEA, https://doi.org/10.1594/PANGAEA.261498
Always quote citation above when using data! You can download the citation in several formats below.
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
Weaver, Barry L; Rideout, M L; Neuser, R D; Khan, Mohammad Javed; Hill, Ian Ashley; Echols, D J; Drake, N; Curtis, Doris M; Clark, Murlene W; Christie, David M; Brannon, Joyce C; Mills, William; Bougault, Henri; Cande, Steven C (1985): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXXXII, 667 pp, https://doi.org/10.2973/dsdp.proc.82.1985
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 37.770000 * Longitude: -37.343500
Date/Time Start: 1981-10-03T00:00:00 * Date/Time End: 1981-10-03T00:00:00
Minimum DEPTH, sediment/rock: 408.53 m * Maximum DEPTH, sediment/rock: 545.10 m
Event(s):
82-558 * Latitude: 37.770000 * Longitude: -37.343500 * Date/Time: 1981-10-03T00:00:00 * Elevation: -3754.0 m * Penetration: 561.5 m * Recovery: 237.8 m * Location: North Atlantic/RIDGE * Campaign: Leg82 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 43 cores; 394.5 m cored; 0 m drilled; 60.3 % 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 | Smith, Guy M | DSDP/ODP/IODP sample designation | ||
3 | Sample ID | Sample ID | Smith, Guy M | |||
4 | Lithology/composition/facies | Lithology | Smith, Guy M | |||
5 | NRM, Intensity | Inten (NRM) | mA/m | Smith, Guy M | reviewed and corrected (x 1000) by PANGAEA | |
6 | NRM, Inclination | Incl (NRM) | deg | Smith, Guy M | ||
7 | NRM, Declination | Decl (NRM) | deg | Smith, Guy M | ||
8 | NRM, median destructive field of natural remanent magnetization, alternating field | MDF (NRM) | mT | Smith, Guy M | ||
9 | Magnetic susceptibility, volume | kappa | 10-6 SI | Smith, Guy M | Initial susceptibility [gauss/oersteds] transformed to 10**-6 SI | |
10 | Koenigsberger ratio | Q-ratio | A/m | Smith, Guy M | ||
11 | Sample method | Sample method | Smith, Guy M | Thermomagnetic curve | ||
12 | Curie temperature | Curie temp | °C | Smith, Guy M | ||
13 | Hysteresis, saturation magnetization, per unit volume | Ms | mA/m | Smith, Guy M | ||
14 | Hysteresis, saturation remanence, per unit volume | Msr | mA/m | Smith, Guy M | ||
15 | Coercive force | Bc | mT | Smith, Guy M | ||
16 | Coercivity of remanence | Bcr | mT | Smith, Guy M | Remanent coercive force | |
17 | Comment | Comment | Smith, Guy M |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
614 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 MDF (NRM) [mT] | 9 kappa [10-6 SI] | 10 Q-ratio [A/m] | 11 Sample method | 12 Curie temp [°C] | 13 Ms [mA/m] | 14 Msr [mA/m] | 15 Bc [mT] | 16 Bcr [mT] | 17 Comment |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
408.53 | 82-558-27-3,51-54 | 6 | Igneous | 0.370 | -51.00 | 69.0 | 1.13 | 8.200 | Curie temperature is from the cooling curve | 570 | BASALT,ALT MOD,PILLOW MARGIN,MULTICOMPONENT | |||||
408.53 | 82-558-27-3,51-54 | 6 | Igneous | Curie temperature is from the heating curve | 340 | 0.1220 | 0.05010 | 18.90 | 29.7 | MAGNETIZATION | ||||||
409.25 | 82-558-27-3,123-126 | 11B | Igneous | 1.810 | -45.00 | 40.5 | 1.56 | 29.200 | Curie temperature is from the cooling curve | 445 | BASALT,ALT MOD,PILLOW INTERIOR | |||||
409.25 | 82-558-27-3,123-126 | 11B | Igneous | Curie temperature is from the heating curve | 265 | 0.1830 | 0.09170 | 17.30 | 24.7 | |||||||
415.03 | 82-558-28-1,52-54 | 5 | Igneous | 0.290 | -70.20 | 101.00 | 0.67 | 12.100 | APHYRIC BASALT,ALT FRESH TO MOD | |||||||
417.53 | 82-558-28-3,2-4 | 1 | Igneous | 0.250 | 3.30 | 130.70 | 1.19 | 5.740 | APHYRIC BASALT,ALT FRESH TO MOD | |||||||
417.61 | 82-558-28-3,9-12 | 1 | Igneous | 0.419 | -20.00 | 73.9 | 1.42 | 7.400 | Curie temperature is from the cooling curve | 565 | FRACTURED APHYRIC BASALT(PILLOWS?),ALT MOD,PILLOW | |||||
417.61 | 82-558-28-3,9-12 | 1 | Igneous | Curie temperature is from the heating curve | 350 | 0.0732 | 0.03660 | 29.80 | 45.6 | MARGIN,MULTICOMPONENT MAGNETIZATION | ||||||
417.95 | 82-558-28-3,43-47 | 5 | Igneous | 2.050 | -23.00 | 24.8 | 9.11 | 18.200 | Curie temperature is from the cooling curve | 545 | FRACTURED APHYRIC BASALT(PILLOWS?),ALT FRESH TO | |||||
417.95 | 82-558-28-3,43-47 | 5 | Igneous | Curie temperature is from the heating curve | 295 | 0.1160 | 0.06930 | 31.70 | 39.8 | MOD,PILLOW INTERIOR | ||||||
424.77 | 82-558-29-1,126-128 | 7C | Igneous | 2.650 | -21.70 | 240.00 | 1.06 | 70.200 | APHYRIC BASALT,ALT FRESH TO MOD,PILLOW | |||||||
426.02 | 82-558-29-2,100-103 | 14 | Igneous | 1.110 | 29.00 | 0.89 | 31.400 | Curie temperature is from the cooling curve | 570 | APHYRIC PILLOW BASALT,ALT MOD,PILLOW MARGIN,MDF | ||||||
426.02 | 82-558-29-2,100-103 | 14 | Igneous | Curie temperature is from the heating curve | 375 | 0.0405 | 0.02020 | 43.10 | IS 61% | |||||||
426.25 | 82-558-29-2,124-126 | 16B | Igneous | 0.760 | 52.40 | 325.90 | 0.89 | 23.700 | APHYRIC BASALT,ALT MOD,PILLOW | |||||||
426.40 | 82-558-29-2,138-141 | 16C | Igneous | 3.630 | 34.00 | 54.1 | 2.17 | 42.000 | Curie temperature is from the cooling curve | 540 | APHYRIC PILLOW BASALT,ALT MOD,PILLOW INTERIOR, | |||||
426.40 | 82-558-29-2,138-141 | 16C | Igneous | Curie temperature is from the heating curve | 320 | 0.1110 | 0.06460 | 27.80 | 31.1 | MULTICOMPONENT MAGNETIZATION | ||||||
426.58 | 82-558-29-3,7-9 | 2 | Igneous | 2.760 | 57.00 | 91.70 | 1.85 | 41.800 | APHYRIC BASALT,ALT MOD,PILLOW | |||||||
427.52 | 82-558-29-3,101-103 | 10B | Igneous | 2.740 | -1.30 | 72.60 | 1.17 | 65.500 | APHYRIC BASALT,ALT MOD,PILLOW | |||||||
428.04 | 82-558-29-4,3-5 | 1 | Volcanic breccia (igneous) | 4.170 | -33.80 | 355.10 | 1.41 | 82.700 | INTERPILLOW BRECCIA,ALT MOD | |||||||
433.26 | 82-558-30-1,72-79 | 9A | Igneous | 3.800 | -39.10 | 357.30 | 1.38 | 76.700 | APHYRIC BASALT,ALT MOD,PILLOW | |||||||
434.13 | 82-558-30-2,12-14 | 1B | Igneous | 1.220 | -46.00 | 81.10 | 1.26 | 16.100 | APHYRIC BASALT,ALT SLIGHT | |||||||
436.32 | 82-558-30-3,81-83 | 9 | Igneous | 2.250 | -41.80 | 139.70 | 1.06 | 59.700 | APHYRIC BASALT,ALT SLIGHT,PILLOW | |||||||
437.66 | 82-558-30-4,65-67 | 4C | Igneous | 2.960 | -30.50 | 206.20 | 1.02 | 81.300 | APHYRIC BASALT,ALT SLIGHT,PILLOW | |||||||
442.07 | 82-558-31-1,56-58 | 5B | Igneous | 3.260 | -35.70 | 270.80 | 0.83 | 109.700 | APHYRIC BASALT,ALT FRESH TO MOD,PILLOW | |||||||
443.98 | 82-558-31-2,97-99 | 7 | Igneous | 4.870 | 38.90 | 271.20 | 0.96 | 141.800 | APHYRIC BASALT,ALT SLIGHT,PILLOW | |||||||
450.66 | 82-558-32-1,15-17 | 2 | Igneous | 1.550 | -35.30 | 5.70 | 0.82 | 52.810 | APHYRIC BASALT,ALT MOD,PILLOW | |||||||
453.55 | 82-558-32-3,4-6 | 1 | Igneous | 5.040 | -40.10 | 355.90 | 1.32 | 106.800 | APHYRIC BASALT,ALT FRESH TO MOD | |||||||
456.21 | 82-558-32-4,120-122 | 12B | Igneous | 2.410 | -24.50 | 207.00 | 1.13 | 59.400 | APHYRIC BASALT,ALT MOD | |||||||
456.82 | 82-558-32-5,30-33 | 1C | Igneous | 2.850 | -39.00 | 47.5 | 1.36 | 52.800 | Curie temperature is from the cooling curve | 560 | APHYRIC BASALT,ALT MOD,FLOW INTERIOR | |||||
456.82 | 82-558-32-5,30-33 | 1C | Igneous | Curie temperature is from the heating curve | 305 | 0.1440 | 0.06660 | 24.70 | 39.9 | |||||||
456.87 | 82-558-32-5,36-38 | 1C | Igneous | 1.850 | -43.30 | 104.20 | 1.01 | 51.320 | APHYRIC BASALT,ALT MOD,MASSIVE | |||||||
457.58 | 82-558-32-5,106-109 | 4A | Igneous | 1.320 | -42.00 | 65.2 | 1.05 | 31.700 | Curie temperature is from the cooling curve | 560 | APHYRIC BASALT,ALT MOD,FLOW MARGIN | |||||
457.58 | 82-558-32-5,106-109 | 4A | Igneous | Curie temperature is from the heating curve | 295 | 0.1030 | 0.05660 | 30.60 | 42.7 | |||||||
459.97 | 82-558-33-1,46-48 | 6 | Igneous | 4.310 | -32.00 | 314.00 | 1.06 | 113.900 | APHYRIC BASALT,ALT MOD,PILLOW | |||||||
461.03 | 82-558-33-2,2-4 | 1A | Igneous | 4.990 | -28.20 | 231.80 | 1.19 | 116.700 | APHYRIC BASALT,ALT MOD,PILLOW | |||||||
463.71 | 82-558-33-3,120-122 | 9C | Igneous | 6.590 | -34.40 | 27.30 | 1.58 | 116.300 | APHYRIC BASALT,ALT MOD,PILLOW | |||||||
468.74 | 82-558-34-1,23-25 | 3A | Igneous | 7.010 | -28.70 | 325.20 | 3.34 | 58.580 | APHYRIC BASALT,ALT MOD,PILLOW INTERIOR | |||||||
479.73 | 82-558-35-2,71-74 | 7 | Igneous | 0.182 | -72.00 | 0.87 | 5.300 | Curie temperature is from the cooling curve | 580 | APHYRIC PILLOW BASALT SEQUENCE,ALT MOD,PILLOW | ||||||
479.73 | 82-558-35-2,71-74 | 7 | Igneous | Curie temperature is from the heating curve | 385 | 0.0266 | 0.01510 | 42.80 | MARGIN,MDF IS 80% | |||||||
480.00 | 82-558-35-2,98-101 | 6A | Igneous | 2.180 | -54.00 | 68.1 | 0.76 | 71.700 | Curie temperature is from the cooling curve | 570 | APHYRIC PILLOW BASALT SEQUENCE,ALT MOD,PILLOW | |||||
480.00 | 82-558-35-2,98-101 | 6A | Igneous | Curie temperature is from the heating curve | 310 | 0.1140 | 0.07030 | 47.20 | 63.6 | INTERIOR | ||||||
489.32 | 82-558-36-2,130-133 | 7A | Igneous | 0.455 | -44.00 | 66.7 | 1.03 | 11.100 | Curie temperature is from the cooling curve | 550 | APHYRIC PILLOW BASALT SEQUENCE,ALT MOD,FLOW | |||||
489.32 | 82-558-36-2,130-133 | 7A | Igneous | Curie temperature is from the heating curve | 360 | 0.0533 | 0.03240 | 35.30 | 54.1 | MARGIN | ||||||
489.70 | 82-558-36-3,18-21 | 1B | Igneous | 7.740 | -51.00 | 68.5 | 1.13 | 172.000 | Curie temperature is from the cooling curve | 580 | APHYRIC BASALT,ALT MOD,FLOW INTERIOR, | |||||
489.70 | 82-558-36-3,18-21 | 1B | Igneous | Curie temperature is from the heating curve | 320 | 0.1430 | 0.08760 | 41.10 | 54.2 | MULTICOMPONENT MAGNETIZATION | ||||||
505.08 | 82-558-38-1,56-59 | 3B | Igneous | 2.340 | -33.00 | 44.4 | 1.57 | 37.400 | Curie temperature is from the cooling curve | 555 | APHYRIC BASALT,ALT MOD,PILLOW MARGIN | |||||
505.08 | 82-558-38-1,56-59 | 3B | Igneous | Curie temperature is from the heating curve | 315 | 0.1590 | 0.07410 | 17.20 | 23.8 | |||||||
506.29 | 82-558-38-2,28-30 | 2 | Igneous | 3.710 | 37.50 | 264.70 | 0.85 | 121.300 | APHYRIC BASALT,ALT MOD,PILLOW | |||||||
506.44 | 82-558-38-2,42-45 | 2 | Igneous | 3.650 | 32.00 | 25.8 | 2.14 | 42.900 | Curie temperature is from the cooling curve | 530 | APHYRIC PILLOW BASALT,ALT MOD,PILLOW INTERIOR | |||||
506.44 | 82-558-38-2,42-45 | 2 | Igneous | Curie temperature is from the heating curve | 295 | 0.2150 | 0.09950 | 20.20 | 27.5 | |||||||
510.28 | 82-558-39-1,127-129 | 8B | Igneous | 2.280 | -27.20 | 14.90 | 0.97 | 65.700 | PILLOW BASALT,ALT MOD | |||||||
510.66 | 82-558-39-2,15-17 | 2A | Igneous | 4.280 | -16.50 | 278.10 | 1.26 | 95.150 | PILLOW BASALT,ALT MOD | |||||||
513.56 | 82-558-39-4,4-7 | 1A | Igneous | 3.310 | -26.00 | 42.1 | 1.31 | 63.700 | Curie temperature is from the cooling curve | 555 | APHYRIC PILLOW BASALT,ALT MOD,POSSIBLE FLOW | |||||
513.56 | 82-558-39-4,4-7 | 1A | Igneous | Curie temperature is from the heating curve | 350 | 0.0964 | 0.04920 | 24.40 | 33.9 | |||||||
514.06 | 82-558-39-4,55-57 | 2E | Igneous | 1.820 | -26.00 | 48.5 | 1.06 | 43.300 | Curie temperature is from the cooling curve | 580 | APHYRIC PILLOW BASALT,ALT MOD,POSSIBLE FLOW | |||||
514.06 | 82-558-39-4,55-57 | 2E | Igneous | Curie temperature is from the heating curve | 320 | 0.0835 | 0.04760 | 28.40 | 39.8 | |||||||
529.06 | 82-558-41-2,54-57 | 4A | Igneous | 0.420 | -41.00 | 16.1 | 11.44 | 0.900 | Curie temperature is from the cooling curve | 565 | PERIDOTITE,ALT EXT,COULD BE SULFIDES(?) | |||||
529.06 | 82-558-41-2,54-57 | 4A | Igneous | Curie temperature is from the heating curve | 550 | 0.9750 | 0.18600 | 11.70 | 19.7 | |||||||
529.13 | 82-558-41-2,61-64 | 4B | Igneous | 0.230 | -41.00 | 21.1 | 14.20 | 0.400 | 0.9280 | 0.13500 | 13.40 | 32.0 | PERIDOTITE,ALT EXT | |||
537.10 | 82-558-42-1,109-112 | 6B | Igneous | 5.390 | 41.00 | 12.9 | 59.31 | 2.300 | Curie temperature is from the cooling curve | 580 | PERIDOTITE,ALT MOD | |||||
537.10 | 82-558-42-1,109-112 | 6B | Igneous | Curie temperature is from the heating curve | 560 | 3.1000 | 0.48000 | 11.30 | 16.5 | |||||||
545.10 | 82-558-43-1,8-11 | 7 | Igneous | 2.620 | 42.00 | 7.4 | 68.36 | 1.000 | Curie temperature is from the cooling curve | 580 | SERPENTINITE GABBRO,ALT MOD | |||||
545.10 | 82-558-43-1,8-11 | 7 | Igneous | Curie temperature is from the heating curve | 565 | 4.0300 | 0.54000 | 9.20 | 18.8 |