(Table S4) Mineral composition of sediment core MD99-2317
Cobertura |
LATITUDE: 68.103000 * LONGITUDE: -27.861500 * DATE/TIME START: 1999-08-01T00:00:00 * DATE/TIME END: 1999-08-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 16.914 m * MAXIMUM DEPTH, sediment/rock: 17.298 m |
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Data(s) |
16/10/2015
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Formato |
text/tab-separated-values, 2394 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.854008 doi:10.1594/PANGAEA.854008 |
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; CALYPSO; Calypso Corer; Carbonates; DEPTH, sediment/rock; East Greenland Shelf basin; F/Us; Halite; Illite; IMAGES V; Iron oxide, FeO; Kalifeldspar; Kaolinite; Marion Dufresne; MD114; MD99-2317; 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 |