Mineralogy of sediment core PS2200-2
Cobertura |
LATITUDE: 85.327700 * LONGITUDE: -14.022000 * DATE/TIME START: 1991-09-16T00:00:00 * DATE/TIME END: 1991-09-16T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 0.30 m |
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Data(s) |
05/02/2004
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Formato |
text/tab-separated-values, 35 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.138261 doi:10.1594/PANGAEA.138261 |
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; Calcium carbonate; DEPTH, sediment/rock; Dolomite; Giant box corer; GKG; Morris Jesup Rise; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Plagioclase; Polarstern; PS19/218; PS19 ARCTIC91; PS2200-2; Quartz; Quartz/Feldspar ratio; Quaternary Environment of the Eurasian North; QUEEN; X-ray diffraction (XRD) |
Tipo |
Dataset |