Mineralogy of sediment core PG1111
| Cobertura |
LATITUDE: 69.548000 * LONGITUDE: 90.211000 * DATE/TIME START: 1993-01-01T00:00:00 * DATE/TIME END: 1993-01-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.24 m * MAXIMUM DEPTH, sediment/rock: 10.60 m |
|---|---|
| Data(s) |
22/10/1999
|
| Formato |
text/tab-separated-values, 154 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.55802 doi:10.1594/PANGAEA.55802 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Harwart, Stefanie K (1999): Geochemische Verwitterungstrends eines basaltischen Ausgangsgesteins nach dem spätpleistozänen Gletscherrückzug auf der Taymyrhalbinsel (Zentralsibirien) - Rekonstruktion an einer sedimentären Abfolge des Lama Sees. (Geochemical weathering trends of a basaltic source rock after the retreat of Late Pleistocene glaciers on the Taymyr Peninsula (Central Siberia) - reconstruction using sedimentary sequences of Lake Lama). Berichte zur Polarforschung = Reports on Polar Research, 324, 123 pp, doi:10.2312/BzP_0324_1999 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Augite; AWI_PerDyn; COMPCORE; Composite Core; DEPTH, sediment/rock; Illite/standard ratio; Kaolinite/standard ratio; Norilsk/Taymyr, Sibiria; Norilsk/Taymyr93; Orthoclase; Periglacial Dynamics @ AWI; PG1111; Plagioclase/standard ratio; Quartz/total intensity ratio; Quaternary Environment of the Eurasian North; QUEEN; Sampling/drilling in lake; Smectite/standard ratio; X-ray diffraction TEXTUR, clay fraction |
| Tipo |
Dataset |
