Day, Ron; Luyendyk, Bruce P; Cann, Joe R (2005): Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 49-412A. PANGAEA, https://doi.org/10.1594/PANGAEA.261406
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
Luyendyk, Bruce P; Cann, Joe R; Sharman, G; Roberts, W P; Shor, A N; Duffield, W A; Varet, J; Zolotarev, Boris P; Poore, Richard Z; Steinmetz, J C; Kobayashi, Kazuo; Vennum, W; Wood, D A; Steiner, M (1979): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XLIX, 1020 pp, https://doi.org/10.2973/dsdp.proc.49.1979
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 36.562300 * Longitude: -33.166000
Date/Time Start: 1976-08-24T00:00:00 * Date/Time End: 1976-08-24T00:00:00
Minimum DEPTH, sediment/rock: 156.30 m * Maximum DEPTH, sediment/rock: 285.81 m
Event(s):
49-412A * Latitude: 36.562300 * Longitude: -33.166000 * Date/Time: 1976-08-24T00:00:00 * Elevation: -2609.0 m * Penetration: 294 m * Recovery: 23.1 m * Location: North Atlantic/FRACTURE ZONE * Campaign: Leg49 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 14 cores; 133 m cored; 5 m drilled; 17.3 % 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 | Day, Ron | DSDP/ODP/IODP sample designation | ||
3 | Sample ID | Sample ID | Day, Ron | |||
4 | Lithology/composition/facies | Lithology | Day, Ron | |||
5 | NRM, Intensity | Inten (NRM) | mA/m | Day, Ron | reviewed and corrected (x 1000) by PANGAEA | |
6 | NRM, Inclination | Incl (NRM) | deg | Day, Ron | ||
7 | ChRM, Inclination | Incl (ChRM) | deg | Day, Ron | ||
8 | NRM, median destructive field of natural remanent magnetization, alternating field | MDF (NRM) | mT | Day, Ron | ||
9 | Magnetic susceptibility, volume | kappa | 10-6 SI | Day, Ron | Initial susceptibility [gauss/oersteds] transformed to 10**-6 SI | |
10 | Koenigsberger ratio | Q-ratio | A/m | Day, Ron | ||
11 | Curie temperature | Curie temp | °C | Day, Ron | ||
12 | Hysteresis, saturation magnetization, per unit volume | Ms | mA/m | Day, Ron | ||
13 | Hysteresis, saturation remanence, per unit volume | Msr | mA/m | Day, Ron | ||
14 | Coercive force | Bc | mT | Day, Ron | ||
15 | Coercivity of remanence | Bcr | mT | Day, Ron | Remanent coercive force | |
16 | Grain size description | Grain size descr | Day, Ron | Grain size given in µm | ||
17 | Comment | Comment | Day, Ron |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
425 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 Incl (ChRM) [deg] | 8 MDF (NRM) [mT] | 9 kappa [10-6 SI] | 10 Q-ratio [A/m] | 11 Curie temp [°C] | 12 Ms [mA/m] | 13 Msr [mA/m] | 14 Bc [mT] | 15 Bcr [mT] | 16 Grain size descr | 17 Comment |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
156.30 | 49-412A-1-1,29-30 | 3 | Igneous | 7.990 | 62.70 | 62.4 | 3.0 | 170 | 1.6600 | 0.23200 | 3.80 | 8.5 | @7-15 | APHYRIC BASALT | ||
156.30 | 49-412A-1-1,29-30 | 3 | Igneous | APHYRIC BASALT,THERMOMAGNETIC CURVE IS | ||||||||||||
156.30 | 49-412A-1-1,29-30 | 3 | Igneous | REVERSIBLE | ||||||||||||
165.62 | 49-412A-2-1,12-12 | 6 | Igneous | 2.800 | -18.40 | -23.9 | 3.5 | PLAG-CLINOPYROXENE-OL PHYRIC MICRODOLERITE | ||||||||
166.03 | 49-412A-2-1,52-54 | 6 | Igneous | 8.26 | 1.1800 | 0.52000 | 19.70 | 28.0 | PLAG-CPX-OL PHYRIC MICRODOLERITE | |||||||
167.36 | 49-412A-2-2,35-37 | Igneous | 2.4 | 29.66 | 1.900 | PLAG-CPX-OL PHYRIC MICRODOLERITE,THERMOMAGNETIC | ||||||||||
167.36 | 49-412A-2-2,35-37 | 1 | Igneous | 1.990 | -5.20 | -55.2 | 3.5 | 178 | 1.8400 | 0.14700 | 3.10 | 7.5 | @10-40 | PLAG-CLINOPYROXENE-OL PHYRIC GABBRO-DOLERITE | ||
167.36 | 49-412A-2-2,35-37 | Igneous | CURVE IS REVERSIBLE | |||||||||||||
175.74 | 49-412A-3-1,73-75 | 9 | Igneous | 1.260 | -10.30 | -46.4 | 6.5 | PLAG-CPX-OL SPARSELY PHYRIC MICRODOLERITE | ||||||||
176.86 | 49-412A-3-2,35-37 | 3 | Igneous | 5.180 | -43.0 | 4.2 | 32.55 | 4.400 | 1.7100 | 0.13700 | 2.70 | 7.7 | PLAG-CPX-OL PHYRIC MICRODOLERITE | |||
177.22 | 49-412A-3-2,71-73 | 4B | Igneous | 1.470 | -5.90 | -73.4 | 4.5 | PLAG-CPX-OL PHYRIC MICRODOLERITE | ||||||||
184.78 | 49-412A-4-1,26-29 | 3 | Igneous | 2.900 | PLAG-OL MOD PHYRIC MICRODOLERITE | |||||||||||
194.53 | 49-412A-5-1,52-54 | 5 | Igneous | 4.350 | -35.60 | -67.0 | 5.0 | PLAG-OL SPARSELY PHYRIC BASALT | ||||||||
203.99 | 49-412A-6-1,48-50 | 5 | Igneous | 6.470 | -38.00 | -51.8 | 13.82 | 13.000 | PLAG-OL SPARSELY PHYRIC BASALT,MDF IS THERMAL | |||||||
213.52 | 49-412A-7-1,52 | 7 | Igneous | 5.000 | -46.0 | 32.5 | 7.33 | 19.000 | 1.2800 | 0.49900 | 15.50 | 23.4 | PLAG-OL SPARSELY PHYRIC BASALT | |||
213.60 | 49-412A-7-1,59-60 | 8 | Igneous | 8.420 | -41.10 | -45.4 | 13.5 | PLAG-OL SPARSELY PHYRIC BASALT,MDF NOT TRUE. | ||||||||
213.60 | 49-412A-7-1,59-60 | 8 | Igneous | HIGHER VALUE ARISES FROM SUPERPOSITION OF | ||||||||||||
213.60 | 49-412A-7-1,59-60 | 8 | Igneous | REVERSED AND NORMAL COMPONENT AND CONCOMITANT | ||||||||||||
213.60 | 49-412A-7-1,59-60 | 8 | Igneous | INTENSITY RISE IN LOW FIELDS,ALT SLIGHT | ||||||||||||
215.11 | 49-412A-7-2,60-62 | 7 | Igneous | 11.5 | 16.46 | 5.600 | HIGHER VALUE ARISE FROM SUPERPOSITION OF | |||||||||
215.11 | 49-412A-7-2,60-62 | 7 | Igneous | 3.280 | -46.90 | -54.5 | 12.5 | 270 | 2.1600 | 0.41000 | 9.00 | 18.2 | @2-15 | PLAG-OL SPARSELY PHYRIC BASALT,MDF NOT TRUE. | ||
215.11 | 49-412A-7-2,60-62 | 7 | Igneous | REVERSED AND NORMAL COMPONENTS AND CONCOMITANT | ||||||||||||
215.11 | 49-412A-7-2,60-62 | 7 | Igneous | INTENSITY RISE IN LOW FIELDS | ||||||||||||
215.11 | 49-412A-7-2,60-62 | 7 | Igneous | PLAG-OL SPARSELY PHYRIC BASALT,THERMOMAGNETIC | ||||||||||||
215.11 | 49-412A-7-2,60-62 | 7 | Igneous | CURVE IS REVERSIBLE | ||||||||||||
223.57 | 49-412A-8-1,106-108 | 14 | Igneous | 8.790 | PLAG-OL SPARSELY PHYRIC BASALT | |||||||||||
224.29 | 49-412A-8-2,28-30 | 4A | Igneous | 1.390 | -2.10 | -47.4 | 6.0 | PLAG-OL SPARSELY PHYRIC BASALT | ||||||||
232.49 | 49-412A-9-1,48-50 | 6 | Igneous | 18.60 | 8.800 | PLAG-OL SPARSELY PHYRIC BASALT,THERMOMAGNETIC | ||||||||||
232.49 | 49-412A-9-1,48-50 | 6 | Igneous | 5.880 | -43.60 | -51.7 | 9.5 | 205 | 1.4000 | 0.39200 | 6.50 | 13.1 | PLAG-OL SPARSELY PHYRIC BASALT | |||
232.49 | 49-412A-9-1,48-50 | 6 | Igneous | CURVE IS REVERSIBLE | ||||||||||||
241.90 | 49-412A-10-1,39-41 | 4 | Igneous | 2.870 | -53.30 | -67.1 | 6.0 | 17.59 | 3.000 | 2.5100 | 0.26600 | 3.10 | 6.5 | APHYRIC BASALT | ||
241.90 | 49-412A-10-1,39-41 | 4 | Igneous | 34.81 | 2.300 | APHYRIC BASALT | ||||||||||
251.55 | 49-412A-11-1,54-56 | 7 | Igneous | 1.210 | -49.50 | -56.1 | 7.0 | APHYRIC BASALT | ||||||||
252.82 | 49-412A-11-2,31-33 | 3 | Igneous | 0.728 | -56.90 | -58.4 | 8.0 | 15.08 | 2.000 | PLAG-OL SPARSELY PHYRIC BASALT | ||||||
253.00 | 49-412A-11-2,50 | 4 | Igneous | 1.700 | -63.0 | 8.6 | 28.78 | 1.600 | 1.7600 | 0.14100 | 2.80 | 8.0 | PLAG-OL SPARSELY PHYRIC BASALT | |||
254.70 | 49-412A-11-3,69-71 | 7 | Igneous | 23.62 | 4.400 | VALUE ARISES FROM SUPERPOSITION OF REVERSED AND | ||||||||||
254.70 | 49-412A-11-3,69-71 | 7 | Igneous | 3.720 | -67.50 | -66.4 | 15.0 | 210 | 1.7600 | 0.26400 | 5.50 | 11.5 | 0.5-5 | PLAG SPARSELY PHYRIC BASALT,MDF NOT TRUE.HIGHER | ||
254.70 | 49-412A-11-3,69-71 | 7 | Igneous | NORMAL COMPONENTS AND CONCOMITANT INTENSITY RISE | ||||||||||||
254.70 | 49-412A-11-3,69-71 | 7 | Igneous | IN LOW FIELDS | ||||||||||||
254.70 | 49-412A-11-3,69-71 | 7 | Igneous | PLAG SPARSELY PHYRIC BASALT,THERMOMAGNETIC CURVE | ||||||||||||
254.70 | 49-412A-11-3,69-71 | 7 | Igneous | IS REVERSIBLE | ||||||||||||
270.29 | 49-412A-13-1,28-30 | 2B | Igneous | 2.730 | -16.60 | -35.1 | 9.5 | APHYRIC BASALT | ||||||||
272.03 | 49-412A-13-2,52-54 | 5 | Igneous | 5.340 | APHYRIC BASALT | |||||||||||
272.30 | 49-412A-13-2,79-81 | 7A | Igneous | 5.060 | -33.30 | -45.1 | 13.0 | APHYRIC BASALT,ALT EXT | ||||||||
273.90 | 49-412A-13-3,89-91 | 9 | Igneous | 0.627 | -42.2 | 13.0 | PLAG-OL SPARSELY PHYRIC BASALT | |||||||||
279.63 | 49-412A-14-1,12-14 | 1 | Igneous | 2.360 | -38.40 | -53.0 | 8.0 | 22.62 | 3.100 | 1.4900 | 0.14900 | 2.30 | 6.5 | PLAG SPARSELY PHYRIC BASALT | ||
279.63 | 49-412A-14-1,12-14 | 1 | Igneous | 43.23 | 1.500 | PLAG SPARSELY PHYRIC BASALT | ||||||||||
279.95 | 49-412A-14-1,45 | 5 | Igneous | 15.900 | -50.0 | 13.5 | 22.75 | 20.000 | 2.3100 | 0.30000 | 6.20 | 14.0 | PLAG SPARSELY PHYRIC BASALT | |||
282.00 | 49-412A-14-2,99-101 | 10 | Igneous | 1.940 | 3.90 | -53.9 | 3.0 | 185 | 1.8200 | 0.10900 | 1.70 | 17.0 | APHYRIC BASALT | |||
282.00 | 49-412A-14-2,99-101 | 10 | Igneous | APHYRIC BASALT,THERMOMAGNETIC CURVE IS | ||||||||||||
282.00 | 49-412A-14-2,99-101 | 10 | Igneous | REVERSIBLE | ||||||||||||
283.31 | 49-412A-14-3,80-82 | 4B | Igneous | 3.470 | APHYRIC BASALT | |||||||||||
285.07 | 49-412A-14-4,105-108 | 12 | Igneous | 5.080 | -37.30 | -47.6 | 7.0 | APHYRIC BASALT | ||||||||
285.81 | 49-412A-14-5,30-32 | 3 | Igneous | 6.5 | 26.64 | 83.000 | APHYRIC BASALT,THERMOMAGNETIC CURVE IS | |||||||||
285.81 | 49-412A-14-5,30-32 | 3 | Igneous | 0.794 | -1.30 | -70.5 | 7.5 | 200 | 3.7000 | 0.11100 | 1.80 | 7.5 | APHYRIC BASALT | |||
285.81 | 49-412A-14-5,30-32 | 3 | Igneous | REVERSIBLE |