Geochemistry of sediment core GeoB3718-4
| Cobertura |
LATITUDE: -24.895000 * LONGITUDE: 13.160000 * DATE/TIME START: 1996-02-11T00:00:00 * DATE/TIME END: 1996-02-11T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.0025 m * MAXIMUM DEPTH, sediment/rock: 0.1750 m |
|---|---|
| Data(s) |
11/02/2009
|
| Formato |
text/tab-separated-values, 72 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.712500 doi:10.1594/PANGAEA.712500 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Zabel, Matthias; Bickert, Torsten; Dittert, Lars; Haese, Ralf R (1999): Significance of the sedimentary Al : Ti ratio as an indicator for variations in the circulation patterns of the equatorial North Atlantic. Paleoceanography, 14(6), 789-799, doi:10.1029/1999PA900027 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Calcium; Carbon, inorganic, total; Carbon, organic, total; DEPTH, sediment/rock; Element analyser CHN, LECO; GeoB; GeoB3718-4; Geosciences, University of Bremen; HF/HNO3/H2O2 pressure digestion; Iron; M34/2; Manganese; Meteor (1986); MUC; MultiCorer; Northern Cape Basin; Phosphate |
| Tipo |
Dataset |
