(Table 2) Clay mineral abundances of sediment cores from the Gulf of Cadiz and the Portuguese margin
| Cobertura |
MEDIAN LATITUDE: 37.741667 * MEDIAN LONGITUDE: -9.143889 * SOUTH-BOUND LATITUDE: 36.380000 * WEST-BOUND LONGITUDE: -10.680000 * NORTH-BOUND LATITUDE: 39.040000 * EAST-BOUND LONGITUDE: -7.071667 * DATE/TIME START: 1997-04-24T14:30:00 * DATE/TIME END: 1997-05-04T18:14:00 * MINIMUM DEPTH, sediment/rock: 0.005 m * MAXIMUM DEPTH, sediment/rock: 5.670 m |
|---|---|
| Data(s) |
18/01/2011
|
| Formato |
text/tab-separated-values, 164 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.774224 doi:10.1594/PANGAEA.774224 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.774225 Stumpf, Roland; Frank, Martin; Schönfeld, Joachim; Haley, Brian A (2011): Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum. Earth and Planetary Science Letters, 312(1-2), 80-90, doi:10.1016/j.epsl.2011.10.002 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Chlorite; DEPTH, sediment/rock; Event label; Gravity corer (Kiel type); Illite; Kaolinite; M39/1; M39/1_08-3; M39/1_36-4; M39/1_58-2; M39008-3; M39058-2; Meteor (1986); SL; Smectite; X-ray diffraction, clay fraction |
| Tipo |
Dataset |
