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Schmieder, Frank (2004): Paleomagnetic analysis of sediment core GeoB6425-2. PANGAEA, https://doi.org/10.1594/PANGAEA.219503

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Related to:
Schmieder, Frank (2004): Magnetic signals in Plio-Pleistocene sediments of the South Atlantic: Chronostratigraphic usability and paleooceanographic implications. In: Wefer, G; Mulitza, S & Ratmeyer, V (eds.), The South Atlantic in the Late Quaternary: Reconstruction of Material Budgets and Current Systems, Springer, Berlin, Heidelberg, New York, 261-277, https://doi.org/10.1007/978-3-642-18917-3_13
Project(s):
South Atlantic in Late Quaternary: Reconstruction of Budget and Currents (SFB261)
Coverage:
Latitude: -33.825200 * Longitude: -23.587300
Date/Time Start: 2000-03-02T08:02:00 * Date/Time End: 2000-03-02T08:02:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 10.70 m
Event(s):
GeoB6425-2 * Latitude: -33.825200 * Longitude: -23.587300 * Date/Time: 2000-03-02T08:02:00 * Elevation: -4352.0 m * Recovery: 10.89 m * Location: Central South Atlantic * Campaign: M46/4 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: geology and geophysics, CTD at 50 m
Comment:
Demagnetization was performed at 5, 10, 15, 20, (25), 30, (35), 40, (45), 50, 65, 80, (95, 100, 110, 120) mT
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepthmGeocode
2ChRM, InclinationIncl (ChRM)degSchmieder, FrankSingle sample demagnetization
3ChRM, DeclinationDecl (ChRM)degSchmieder, FrankSingle sample demagnetization
Size:
424 data points

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