Paleomagnetic analysis of sediment core GeoB1036-1
| Cobertura |
LATITUDE: -21.173333 * LONGITUDE: 3.328333 * DATE/TIME START: 1988-03-05T00:00:00 * DATE/TIME END: 1988-03-05T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.11 m * MAXIMUM DEPTH, sediment/rock: 10.72 m |
|---|---|
| Data(s) |
25/01/2002
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| Formato |
text/tab-separated-values, 596 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.66719 doi:10.1594/PANGAEA.66719 |
| 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 | #Angola Basin; ChRM, Declination; ChRM, Inclination; ChRM, Polarity; DEPTH, sediment/rock; GeoB; GeoB1036-1; Geosciences, University of Bremen; Gravity corer (Kiel type); M6/6; Meteor (1986); NRM, Intensity; NRM, median destructive field, summarize of cumulative partial NRM, AF demag; Single sample demagnetization; SL |
| Tipo |
Dataset |
