Paleomagnetic analysis of sediment core GeoB1413-4
Cobertura |
LATITUDE: -15.680000 * LONGITUDE: -9.455000 * DATE/TIME START: 1991-04-17T00:00:00 * DATE/TIME END: 1991-04-17T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.05 m * MAXIMUM DEPTH, sediment/rock: 10.00 m |
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Data(s) |
25/01/2002
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Formato |
text/tab-separated-values, 515 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.66737 doi:10.1594/PANGAEA.66737 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
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, doi:10.1007/978-3-642-18917-3_13 Thießen, Wolfgang (1993): Magnetische Eigenschaften von Sedimenten des östlichen Südatlantiks und ihre Paläozeanographische Relevanz. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 41, 170 pp, urn:nbn:de:gbv:46-ep000101793 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #ChRM, Declination; ChRM, Inclination; ChRM, Polarity; DEPTH, sediment/rock; GeoB; GeoB1413-4; Geosciences, University of Bremen; Gravity corer (Kiel type); M16/1; Meteor (1986); NRM, Intensity; NRM, median destructive field, summarize of cumulative partial NRM, AF demag; Single sample demagnetization; SL; West Angola Basin |
Tipo |
Dataset |