Al, Ba, Ti of sediment core GeoB2910-1
| Cobertura |
LATITUDE: 4.845000 * LONGITUDE: -21.053333 * DATE/TIME START: 1994-08-26T00:00:00 * DATE/TIME END: 1994-08-26T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.020 m * MAXIMUM DEPTH, sediment/rock: 5.450 m |
|---|---|
| Data(s) |
22/06/1999
|
| Formato |
text/tab-separated-values, 297 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.55376 doi:10.1594/PANGAEA.55376 |
| 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; GeoB2910-1; Geosciences, University of Bremen; Gravity corer (Kiel type); HF/HNO3/H2O2 pressure digestion; M29/3; Meteor (1986); SFB261; Sierra Leone Rise; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Titanium |
| Tipo |
Dataset |
