Clay mineralogy of sediment core PS2202-4
Cobertura |
LATITUDE: 85.108500 * LONGITUDE: -14.368700 * DATE/TIME START: 1991-09-18T00:00:00 * DATE/TIME END: 1991-09-18T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 0.17 m |
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Data(s) |
04/02/2004
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Formato |
text/tab-separated-values, 96 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.137772 doi:10.1594/PANGAEA.137772 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.778039 Vogt, Christoph (1997): Zeitliche und räumliche Verteilung von Mineralvergesellschaftungen in spätquartären Sedimenten des Arktische Ozeans und ihre Nützlichkeit als Klimaindikatoren während der Glazial/Interglazial-Wechsel (Regional and temporal variations of mineral assemblages in Arctic Ocean sediments as climate indicator during glacial/interglacial changes). Berichte zur Polarforschung = Reports on Polar Research, 251, 309 pp, doi:10.2312/BzP_0251_1997 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #ARK-VIII/3; AWI_Paleo; Chlorite; DEPTH, sediment/rock; Feldspar/standard ratio; Illite; Illite 5Å/10Å Esquevin-index; Illite half height width, glycolized; Kaolinite; Morris Jesup Rise; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/222; PS19 ARCTIC91; PS2202-4; Quartz; Quartz/standard ratio; Quaternary Environment of the Eurasian North; QUEEN; Smectite; Smectite, integral width; Smectite (Half height width); X-ray diffraction TEXTUR, clay fraction |
Tipo |
Dataset |