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Schmieder, Frank (2004): Susceptibility versus depth and age of sediment core GeoB3724-4. PANGAEA, https://doi.org/10.1594/PANGAEA.219633

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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: -26.136667 * Longitude: 8.926667
Date/Time Start: 1996-02-15T00:00:00 * Date/Time End: 1996-02-15T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 11.22 m
Event(s):
GeoB3724-4 * Latitude: -26.136667 * Longitude: 8.926667 * Date/Time: 1996-02-15T00:00:00 * Elevation: -4763.0 m * Recovery: 11.41 m * Location: Northern Cape Basin * Campaign: M34/2 * Basis: Meteor (1986) * Device: Gravity corer (Kiel type) (SL) * Comment: FGB
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethodComment
1DEPTH, sediment/rockDepthmGeocode
2AGEAgeka BPGeocode
3Susceptibility, volumekappa10-6 SISchmieder, FrankBartington MS2F spot sensor
Size:
1105 data points

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