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Schmieder, Frank (2004): Susceptibility versus depth and age of sediment core GeoB5112-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219634

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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
Coverage:
Latitude: -23.825000 * Longitude: -16.258333
Date/Time Start: 1998-04-29T16:32:00 * Date/Time End: 1998-04-29T16:32:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 5.94 m
Event(s):
GeoB5112-4 * Latitude: -23.825000 * Longitude: -16.258333 * Date/Time: 1998-04-29T16:32:00 * Elevation: -3842.0 m * Recovery: 5.59 m * Location: Brazil Basin * Campaign: M41/3 (06MT41_3) * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 38 cm sediment recovered from the bomb, cc: foram bearing nannofossil ooze, silty, light brown
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2AGEAgeka BPGeocode
3Magnetic susceptibility, volumekappa10-6 SISchmieder, FrankBartington MS2F spot sensor
Size:
587 data points

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