Facey, D; Anderson, Roger N; Honnorez, Jose J (2005): Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 83-504B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.261505
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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
Newmark, Robin L; Mottl, Michael J; Laverne, Christine; Kinoshita, Hajimu; Kempton, Pamela D; Emmermann, Rolf; Alt, Jeffrey C; Adamson, Andrew C; Anderson, Roger N; Honnorez, Jose J; Becker, K (1985): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXXXIII, 539 pp, https://doi.org/10.2973/dsdp.proc.83.1985
Further details:
Igneous and metamorphic rocks data file - background and methods. hdl:10013/epic.32349.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 1.227200 * Longitude: -83.730200
Date/Time Start: 1981-11-22T00:00:00 * Date/Time End: 1982-01-02T00:00:00
Minimum DEPTH, sediment/rock: 836.18 m * Maximum DEPTH, sediment/rock: 1332.29 m
Event(s):
83-504B * Latitude: 1.227200 * Longitude: -83.730200 * Date/Time Start: 1981-11-22T00:00:00 * Date/Time End: 1982-01-02T00:00:00 * Elevation: -3460.0 m * Penetration: 1350 m * Recovery: 107.7 m * Campaign: Leg83 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: Leg 83 of DSDP was devoted entirely to coring and experiments in Hole 504B, the deepest borehole to date into the oceanic crust. Hole 504B now extends over a kilometer into basement, nearly twice as far as any other DSDP hole, and it is the only DSDP hole to have clearly penetrated into the intrusive sheeted dikes that underlie the extrusive pillow lavas of the upper oceanic crust. At Hole 504B, Leg 83 continued an ongoing DSDP effort that began during Legs 68, 69, and 70 in 1979, and also included part of Leg 92 in 1983. 71 cores; 514 m cored; 0 m drilled; 21 % 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 | Facey, D | DSDP/ODP/IODP sample designation | ||
3 | Sample ID | Sample ID | Facey, D | |||
4 | Lithology/composition/facies | Lithology | Facey, D | |||
5 | NRM, Intensity | Inten (NRM) | mA/m | Facey, D | reviewed and corrected (x 1000) by PANGAEA | |
6 | NRM, Inclination | Incl (NRM) | deg | Facey, D | ||
7 | ChRM, Inclination | Incl (ChRM) | deg | Facey, D | ||
8 | NRM, median destructive field of natural remanent magnetization, alternating field | MDF (NRM) | mT | Facey, D | ||
9 | Magnetic susceptibility, volume | kappa | 10-6 SI | Facey, D | Initial susceptibility [gauss/oersteds] transformed to 10**-6 SI | |
10 | Koenigsberger ratio | Q-ratio | A/m | Facey, D | ||
11 | Sample method | Sample method | Facey, D | Thermomagnetic curve | ||
12 | Curie temperature | Curie temp | °C | Facey, D | ||
13 | Hysteresis, saturation magnetization, per unit volume | Ms | mA/m | Facey, D | ||
14 | Hysteresis, saturation remanence, per unit volume | Msr | mA/m | Facey, D | ||
15 | Coercive force | Bc | mT | Facey, D | ||
16 | Coercivity of remanence | Bcr | mT | Facey, D | Remanent coercive force | |
17 | Comment | Comment | Facey, D |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2004 data points
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