Clay mineralogy of sediment core PS2200-4


Autoria(s): Vogt, Christoph
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: 0.20 m

Data(s)

04/02/2004

Formato

text/tab-separated-values, 132 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.137769

doi:10.1594/PANGAEA.137769

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; PS19/218; PS19 ARCTIC91; PS2200-4; 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