Geochemistry of sediment core GeoB1028-5
| Cobertura |
LATITUDE: -20.104000 * LONGITUDE: 9.185833 * DATE/TIME START: 1988-03-02T00:00:00 * DATE/TIME END: 1988-03-02T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.18 m * MAXIMUM DEPTH, sediment/rock: 10.73 m |
|---|---|
| Data(s) |
25/01/1999
|
| Formato |
text/tab-separated-values, 830 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.54792 doi:10.1594/PANGAEA.54792 |
| 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; DEPTH, sediment/rock; GeoB; GeoB1028-5; Geosciences, University of Bremen; Gravity corer (Kiel type); HF/HNO3/H2O2 pressure digestion; Iron; M6/6; Meteor (1986); SL; Titanium; Walvis Ridge, Southeast Atlantic Ocean |
| Tipo |
Dataset |
