Geochemistry of sediment core GeoB1505-2
| Cobertura |
LATITUDE: 2.266667 * LONGITUDE: -33.015000 * DATE/TIME START: 1991-05-03T00:00:00 * DATE/TIME END: 1991-05-03T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.025 m * MAXIMUM DEPTH, sediment/rock: 8.575 m |
|---|---|
| Data(s) |
23/06/1999
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| Formato |
text/tab-separated-values, 1935 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.55378 doi:10.1594/PANGAEA.55378 |
| 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 | #Age model; Age model, SPECMAP chronology, Imbrie et al. (1984); Aluminium; Barium; Brazil Basin; Calcium carbonate; Calculated from weight/volume; Carbon, organic, total; Cibicidoides wuellerstorfi, d18O; Density, dry bulk; DEPTH, sediment/rock; Element analyser CHN; Element analyser CHN, LECO; GeoB; GeoB1505-2; Geosciences, University of Bremen; Gravity corer (Kiel type); HF/HNO3/H2O2 pressure digestion; Iron; M16/2; Magnesium; Manganese; Mass spectrometer Finnigan MAT 251; Meteor (1986); Potassium; SL; Titanium |
| Tipo |
Dataset |
