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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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Project(s):
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):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Latitude of eventLatitude
3Longitude of eventLongitude
4Elevation of eventElevationm
5Sample code/labelSample labelVerma, Surendra PDSDP/ODP/IODP sample designation
6Saturation magnetizationJsemu/gVerma, Surendra P
7Remanent saturation magnetizationJrsemu/gVerma, Surendra P
8RatioRatioVerma, Surendra PSaturation remanent magnetization/saturation magnetization ratio
9CoercivityHcOeVerma, Surendra P
10Coercivity of remanenceHcrOeVerma, Surendra P
11Coercivity of remanence/coercive forceBcr/BcVerma, Surendra P
12SusceptibilitySusceptsensor valuesVerma, Surendra PStrong field initial susceptibility; Unit is 10**-3emu/g*Oe
13SusceptibilitySusceptsensor valuesVerma, Surendra PStrong field susceptibility (mean slope of saturation curve); Unit is 10**-5emu/g*Oe
14RatioRatioVerma, Surendra PStrong field initial susceptibility/Strong field susceptibility (mean slope of saturation curve) ratio
15Curie temperatureCurie temp°CVerma, Surendra P
16CommentCommentVerma, Surendra P
Size:
127 data points

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