Verma, Surendra P (1982): (Table 2) Hysteresis and thermomagnetic characteristics of DSDP Leg 64 Holes igneous rocks [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.818520, In supplement to: Verma, SP (1982): Magnetic properties and incompatible element geochemistry of some igneous rocks from Deep Sea Drilling Project Leg 64. In: Curray, JR; Moore, DG; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 64, 667-671, https://doi.org/10.2973/dsdp.proc.64.115.1982
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Published: 1982 (exact date unknown) • DOI registered: 2013-09-26
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 26.084775 * Median Longitude: -110.848000 * South-bound Latitude: 22.959300 * West-bound Longitude: -111.507700 * North-bound Latitude: 27.253000 * East-bound Longitude: -108.978000
Date/Time Start: 1978-12-02T00:00:00 * Date/Time End: 1979-01-03T00:00:00
Minimum Elevation: -3022.0 m * Maximum Elevation: -1889.0 m
Event(s):
64-474A * Latitude: 22.959300 * Longitude: -108.978000 * Date/Time: 1978-12-02T00:00:00 * Elevation: -3022.0 m * Penetration: 626 m * Recovery: 290.1 m * Location: North Pacific/Gulf of California/BASIN * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 49 cores; 453 m cored; 9.5 m drilled; 64 % recovery
64-477A * Latitude: 27.030000 * Longitude: -111.398800 * Date/Time: 1978-12-18T00:00:00 * Elevation: -2003.0 m * Penetration: 267 m * Recovery: 16 m * Location: North Pacific/Gulf of California/BASIN * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 111 m cored; 9.5 m drilled; 14.4 % recovery
64-478 * Latitude: 27.096800 * Longitude: -111.507500 * Date/Time: 1978-12-24T00:00:00 * Elevation: -1889.0 m * Penetration: 464 m * Recovery: 297.6 m * Location: North Pacific/Gulf of California/CHANNEL * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 49 cores; 427 m cored; 24 m drilled; 69.7 % recovery
Comment:
The first row (heating cycle) of hysteresis data pertains to the unheated (original) sample. The second row (cooling cycle) of data corresponds to the sample heated to obtain thermomagnetic curves. For Sample 64-477A-2-2,8-10, the first two rows of data pertain to unheated samples and show the reproducibility of measurements.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | Sample code/label | Sample label | Verma, Surendra P | DSDP/ODP/IODP sample designation | ||
| 6 | Saturation magnetization | Js | emu/g | Verma, Surendra P | ||
| 7 | Remanent saturation magnetization | Jrs | emu/g | Verma, Surendra P | ||
| 8 | Ratio | Ratio | Verma, Surendra P | Saturation remanent magnetization/saturation magnetization ratio | ||
| 9 | Coercivity | Hc | Oe | Verma, Surendra P | ||
| 10 | Coercivity of remanence | Hcr | Oe | Verma, Surendra P | ||
| 11 | Coercivity of remanence/coercive force | Bcr/Bc | Verma, Surendra P | |||
| 12 | Susceptibility | Suscept | sensor values | Verma, Surendra P | Strong field initial susceptibility; Unit is 10**-3emu/g*Oe | |
| 13 | Susceptibility | Suscept | sensor values | Verma, Surendra P | Strong field susceptibility (mean slope of saturation curve); Unit is 10**-5emu/g*Oe | |
| 14 | Ratio | Ratio | Verma, Surendra P | Strong field initial susceptibility/Strong field susceptibility (mean slope of saturation curve) ratio | ||
| 15 | Curie temperature | Curie temp | °C | Verma, Surendra P | ||
| 16 | Comment | Comment | Verma, Surendra P |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
127 data points