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Dmitriev, Yuri I (1982): (Table 5) Titanomagnetite in basalts DSDP Hole 66-487 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817778, In supplement to: Dmitriev, YI (1982): Petrology and origin of basalts of the Middle America Trench, southern Mexico Transect. In: Watkins, JS; Casey Moore, J; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 66, 703-710, https://doi.org/10.2973/dsdp.proc.66.133.1982

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Project(s):
Coverage:
Latitude: 15.853500 * Longitude: -99.175300
Date/Time Start: 1979-03-24T00:00:00 * Date/Time End: 1979-03-24T00:00:00
Minimum Elevation: -4764.0 m * Maximum Elevation: -4764.0 m
Event(s):
66-487 * Latitude: 15.853500 * Longitude: -99.175300 * Date/Time: 1979-03-24T00:00:00 * Elevation: -4764.0 m * Penetration: 190.5 m * Recovery: 119.6 m * Location: North Pacific/TRENCH * Campaign: Leg66 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 180.5 m cored; 9.5 m drilled; 66.3 % recovery
Comment:
The determination of the unit cell dimension of magnetic ore mineral from Sample 66-487-20-1,113-115 cm, performed by M. T. Dmitrieva, shows that according to the value of this parameter, a = 8.405 ± 0.005 Å, the mineral is almost pure magnetite (a = 8.395-8.40 Å).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelDmitriev, Yuri IDSDP/ODP/IODP sample designation
2DescriptionDescriptionDmitriev, Yuri I
3Silicon dioxideSiO2%Dmitriev, Yuri IElectron microprobe (EMP)
4Titanium dioxideTiO2%Dmitriev, Yuri IElectron microprobe (EMP)
5Aluminium oxideAl2O3%Dmitriev, Yuri IElectron microprobe (EMP)
6Iron oxide, FeOFeO%Dmitriev, Yuri IElectron microprobe (EMP)
7Manganese oxideMnO%Dmitriev, Yuri IElectron microprobe (EMP)
8Magnesium oxideMgO%Dmitriev, Yuri IElectron microprobe (EMP)
9Calcium oxideCaO%Dmitriev, Yuri IElectron microprobe (EMP)
10Vanadium oxideV2O5%Dmitriev, Yuri IElectron microprobe (EMP)
11TotalTotal%Dmitriev, Yuri IElectron microprobe (EMP)
Size:
55 data points

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