Relative clay mineral abundances of sediment core GeoB2821-1
| Cobertura |
LATITUDE: -30.451667 * LONGITUDE: -38.801667 * DATE/TIME START: 1994-07-30T00:00:00 * DATE/TIME END: 1994-07-30T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 8.03 m |
|---|---|
| Data(s) |
02/11/1999
|
| Formato |
text/tab-separated-values, 1445 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.55840 doi:10.1594/PANGAEA.55840 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.730524 Gingele, Franz; Schmieder, Frank; von Dobeneck, Tilo; Petschick, Rainer; Rühlemann, Carsten (1999): Terrigenous flux in the Rio Grande Rise area during the last 1.5 Ma: evidence of deepwater advection or rapid response to continental rainfall patterns. Paleoceanography, 14(1), 84-95, doi:10.1029/1998PA900012 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Chlorite; DEPTH, sediment/rock; GeoB; GeoB2821-1; Geosciences, University of Bremen; Gravity corer (Kiel type); Illite; Illite 5Å/10Å Esquevin-index; Illite half height width, glycolized; Kaolinite; Kaolinite/Chlorite ratio; M29/2; Meteor (1986); Quartz/Feldspar ratio; Rio Grande Rise; SL; Smectite; Smectite (Half height width); X-ray diffraction TEXTUR, clay fraction |
| Tipo |
Dataset |
