Geochemistry of sediment core GeoB2809-4
| Cobertura |
LATITUDE: -36.331667 * LONGITUDE: -51.521667 * DATE/TIME START: 1994-07-20T00:00:00 * DATE/TIME END: 1994-07-20T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.1 m * MAXIMUM DEPTH, sediment/rock: 10.3 m |
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| Data(s) |
11/02/2009
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| Formato |
text/tab-separated-values, 360 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.712496 doi:10.1594/PANGAEA.712496 |
| 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 | #Aluminium; Barium; Calcium; Carbon, inorganic, total; Carbon, organic, total; DEPTH, sediment/rock; Element analyser CHN, LECO; GeoB; GeoB2809-4; Geosciences, University of Bremen; Gravity corer (Kiel type); HF/HNO3/H2O2 pressure digestion; Iron; M29/2; Magnesium; Manganese; Meteor (1986); SL; Strontium; Uruguay continental margin |
| Tipo |
Dataset |
