Distribution of minerals in surface sediments of Lake Lama, sites PG1107-1 to PG1122-1
| Cobertura |
MEDIAN LATITUDE: 69.569167 * MEDIAN LONGITUDE: 90.241944 * SOUTH-BOUND LATITUDE: 69.541667 * WEST-BOUND LONGITUDE: 90.175000 * NORTH-BOUND LATITUDE: 69.593333 * EAST-BOUND LONGITUDE: 90.363333 * MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 0.03 m |
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| Data(s) |
20/07/1999
|
| Formato |
text/tab-separated-values, 42 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.55777 doi:10.1594/PANGAEA.55777 |
| 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; Date/Time of event; DEPTH, sediment/rock; Elevation of event; Event label; Feldspar/standard ratio; Gravity corer Potsdam; Illite/standard ratio; Kaolinite/standard ratio; KOL_P; Latitude of event; Longitude of event; Norilsk/Taymyr93; Periglacial Dynamics @ AWI; PG1107-1; PG1108-1; PG1109-1; PG1110-1; PG1114-1; PG1122-1; Piston corer Potsdam; Plagioclase/standard ratio; Quartz/total intensity ratio; Quaternary Environment of the Eurasian North; QUEEN; Sampling/drilling in lake; SL_P; Smectite/standard ratio; X-ray diffraction (XRD); X-ray diffraction TEXTUR, clay fraction |
| Tipo |
Dataset |
