(Table S4) Mineral composition of sediment core HU2008029-070PC
| Cobertura |
LATITUDE: 68.228000 * LONGITUDE: -57.618000 * MINIMUM DEPTH, sediment/rock: 0.050 m * MAXIMUM DEPTH, sediment/rock: 2.250 m |
|---|---|
| Data(s) |
16/10/2015
|
| Formato |
text/tab-separated-values, 418 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.853996 doi:10.1594/PANGAEA.853996 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.854024 Andrews, John T; Bjørk, Anders A; Eberl, Dennis D; Jennings, Anne E; Verplanck, Emily P (2015): Significant differences in late Quaternary bedrock erosion and transport: East versus West Greenland -70°N - evidence from the mineralogy of offshore glacial marine sediments. Journal of Quaternary Science, 30(5), 452-463, doi:10.1002/jqs.2787 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Amphibole; Anorthoclase; Biotite and Chlorite; Carbonates; Davis Strait; DEPTH, sediment/rock; Halite; HU2008029-070PC; HUD08/29; Hudson; Illite; Iron oxide, FeO; Kalifeldspar; Kaolinite; Plagioclase; Principal component analyses (PCA); Principle component 1; Principle component 2; Principle component 3; Principle component 4; Principle component 5; Pyroxene; Quartz; Silica, amorphous; Smectite |
| Tipo |
Dataset |
