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Magnetic data of sediment core MD03-2685
The low-field magnetic susceptibility was measured on u-channels using a 45 mm inner diameter Bartington coil.NRM, IRM and ARM were measured on u-channels using 755R DC-SQUIDS... -
Magnetic data of sediment core MD03-2679
The low-field magnetic susceptibility was measured on u-channels using a 45 mm inner diameter Bartington coil.NRM, IRM and ARM were measured on u-channels using 755R DC-SQUIDS... -
Magnetic data of sediment core MD03-2673
The low-field magnetic susceptibility was measured on u-channels using a 45 mm inner diameter Bartington coil.NRM, IRM and ARM were measured on u-channels using 755R DC-SQUIDS... -
(Table 1) Rock magnetic parameters of core samples obtained from Morne Rouge,...
The magnetic high field susceptibility chi(hifi) indicates the presence of mafic paramagnetic minerals in the scoriae and points to an absence of clay minerals, and in turn of... -
(Table 1) Natural remanent magnetization and magnetic susceptibility of ODP H...
This dataset has no description
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Magnetic susceptibility (Chi) determination from the Jiaxian Section on the C...
This dataset has no description
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Magnetic susceptibility of the late Eocene-early Oligocene interval, southwes...
This dataset has no description
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Volume susceptibility of sediment core SO202/1_45-1
Magnetic volume susceptibility k is the ratio of sample magnetization change per applied external magnetic field change. It is unitless in the SI unit system, which we signalize... -
Volume susceptibility of sediment core SO202/1_44-2
Magnetic volume susceptibility k is the ratio of sample magnetization change per applied external magnetic field change. It is unitless in the SI unit system, which we signalize... -
Volume susceptibility of sediment core SO202/1_43-1
Magnetic volume susceptibility k is the ratio of sample magnetization change per applied external magnetic field change. It is unitless in the SI unit system, which we signalize... -
Volume susceptibility of sediment core SO202/1_42-1
Magnetic volume susceptibility k is the ratio of sample magnetization change per applied external magnetic field change. It is unitless in the SI unit system, which we signalize... -
Volume susceptibility of sediment core SO202/1_41-1
Magnetic volume susceptibility k is the ratio of sample magnetization change per applied external magnetic field change. It is unitless in the SI unit system, which we signalize... -
Volume susceptibility of sediment core SO202/1_39-3
Magnetic volume susceptibility k is the ratio of sample magnetization change per applied external magnetic field change. It is unitless in the SI unit system, which we signalize... -
Volume susceptibility of sediment core SO202/1_38-2
Magnetic volume susceptibility k is the ratio of sample magnetization change per applied external magnetic field change. It is unitless in the SI unit system, which we signalize... -
Sediment characteristics of five cores from a terrestrial permafrost area in ...
Mass specific magnetic susceptibility was measured using a Bartington MS-2 Magnetic Susceptibility System.Grain size composition was determined using a Malvern Mastersizer 3000... -
Sedimentology data from a polygonal tundra landscape near the WWF station Kyt...
Patterned ground of the polygonal tundra yields sensitive indicators of environmental and climate change. Polygon ponds, mires and cryosoils are typical components of Arctic... -
(Table 2) Petrophysical, petrological, and geochemical characteristics of ODP...
Ocean Drilling Program Hole 990A penetrated 131 m of subaerially emplaced Paleocene flood basalts on the Southeast Greenland margin with a recovery of 74%. Shipboard P-wave... -
(Table T1) Magnetic properties of MORB from ODP Leg 187 sites
The core samples of mid-ocean-ridge basalts (including Indian and Pacific type) recovered from the Southeast Indian Ridge (SEIR) area near the Australian Antarctic Discordance...
