(Table S4) Mineral composition of sediment core MD99-2317


Autoria(s): Andrews, John T; Bjørk, Anders A; Eberl, Dennis D; Jennings, Anne E; Verplanck, Emily P
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

Data(s)

16/10/2015

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