Fig. 2: Comparison of the number of grains counted in a sieve analysis
| Cobertura |
LATITUDE: -70.942833 * LONGITUDE: -13.653500 * DATE/TIME START: 1983-03-04T00:00:00 * DATE/TIME END: 1983-03-04T00:00:00 * MINIMUM DEPTH, sediment/rock: 5.28 m * MAXIMUM DEPTH, sediment/rock: 8.27 m |
|---|---|
| Data(s) |
02/02/1987
|
| Resumo |
The distribution of ice rafted debris (IRD) is an important parameter in glaciomarine sediments. A simple method is presented allowing the determination of the IRD-content by counting the gravel fraction of the X-radiographs which are generally taken during sarnpling. In comparison with sieve analyses corresponding values are obtained by both methods. However, more information can be made available in a shorter time by this method. |
| Formato |
text/tab-separated-values, 114 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.756793 doi:10.1594/PANGAEA.756793 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Data from left part of Fig. 2 (URI: doi:10.1594/PANGAEA.50170) |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Grobe, Hannes (1987): A simple method for the determination of ice-rafted debris in sediment cores. Polarforschung, 57(3), 123-126, hdl:10013/epic.29587.d001 |
| Palavras-Chave | #ANT-I/2; AWI_Paleo; DEPTH, sediment/rock; Gravity corer (Kiel type); Ice rafted debris; Kapp Norvegia; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS01; PS01/221; PS1021-1; SL; Stereomicroscope, incident light (Wild M7A/S) |
| Tipo |
Dataset |
