Lowrie, William; Hayes, Dennis E; Frakes, Lawrence A (2005): Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 28-266 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.261359
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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
Webb, Peter-Noel; Wall, Robert E; Piper, David J W; McCollum, D W; Kemp, E M; Kaneps, Ansis G; Ford, Arthur B; Chen, Pei-Hsin; Burns, Derek A; Barrett, Peter J; Hayes, Dennis E; Frakes, Lawrence A (1975): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVIII, 999 pp, https://doi.org/10.2973/dsdp.proc.28.1975
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -56.402200 * Longitude: 110.111700
Date/Time Start: 1973-01-02T00:00:00 * Date/Time End: 1973-01-02T00:00:00
Minimum DEPTH, sediment/rock: 371.44 m * Maximum DEPTH, sediment/rock: 375.05 m
Event(s):
28-266 * Latitude: -56.402200 * Longitude: 110.111700 * Date/Time: 1973-01-02T00:00:00 * Elevation: -4167.0 m * Penetration: 384 m * Recovery: 145 m * Location: Antarctic Ocean/RIDGE * Campaign: Leg28 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 219.5 m cored; 0 m drilled; 66.1 % 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 | Lowrie, William | DSDP/ODP/IODP sample designation | ||
| 3 | Lithology/composition/facies | Lithology | Lowrie, William | |||
| 4 | NRM, Intensity | Inten (NRM) | mA/m | Lowrie, William | reviewed and corrected (x 1000) by PANGAEA | |
| 5 | ChRM, Inclination | Incl (ChRM) | deg | Lowrie, William | ||
| 6 | NRM, median destructive field of natural remanent magnetization, alternating field | MDF (NRM) | mT | Lowrie, William | ||
| 7 | Magnetic susceptibility, volume | kappa | 10-6 SI | Lowrie, William | Initial susceptibility [gauss/oersteds] transformed to 10**-6 SI | |
| 8 | Koenigsberger ratio | Q-ratio | A/m | Lowrie, William | ||
| 9 | Sample method | Sample method | Lowrie, William | Thermomagnetic curve | ||
| 10 | Curie temperature | Curie temp | °C | Lowrie, William | ||
| 11 | Comment | Comment | Lowrie, William |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
61 data points
Data
| 1 Depth sed [m] | 2 Sample label | 3 Lithology | 4 Inten (NRM) [mA/m] | 5 Incl (ChRM) [deg] | 6 MDF (NRM) [mT] | 7 kappa [10-6 SI] | 8 Q-ratio [A/m] | 9 Sample method | 10 Curie temp [°C] | 11 Comment |
|---|---|---|---|---|---|---|---|---|---|---|
| 371.44 | 28-266-23-1,144 | Igneous | 0.260 | -70.5 | 42.2 | 2.43 | 2.000 | Curie temperature is from the cooling curve | 538 | ALT MOD,APHYRIC BASALTIC GLASS,MCW A,CURIE TEMPS |
| 371.44 | 28-266-23-1,144 | Igneous | 0.380 | -72.1 | 69.0 | 2.59 | 2.770 | Curie temperature is from the heating curve | 321 | OF INIT.MAG.MIN. AND FROM COOLING HALF OF CURVE |
| 371.44 | 28-266-23-1,144 | Igneous | ALT MOD,APHYRIC BASALTIC GLASS,MCW B | |||||||
| 375.05 | 28-266-24-1,55 | Igneous | 0.480 | 75.2 | 17.1 | 3.39 | 2.700 | Curie temperature is from the cooling curve | 546 | FROM INIT.MAG.MIN AND FROM COOLING HALF OF CURVE |
| 375.05 | 28-266-24-1,55 | Igneous | 0.400 | 71.0 | 21.2 | 3.44 | 2.210 | Curie temperature is from the cooling curve | 548 | ALT MOD,APHYRIC BASALTIC GLASS,MCW B |
| 375.05 | 28-266-24-1,55 | Igneous | 0.260 | 69.7 | 19.7 | 3.96 | 1.240 | Curie temperature is from the heating curve | 380 | ALT MOD,APHYRIC BASALTIC GLASS,MCW A,CURIE TEMPS |
| 375.05 | 28-266-24-1,55 | Igneous | Curie temperature is from the heating curve | 385 | ALT MOD,APHYRIC BASALTIC GLASS,MCW C,CURIE TEMPS | |||||
| 375.05 | 28-266-24-1,55 | Igneous | OF INIT.MAG.MIN AND FROM COOLING HALF OF CURVE |