Sedimentology of core PG1904
| Cobertura |
LATITUDE: 35.333630 * LONGITUDE: 98.482390 * DATE/TIME START: 2008-03-12T00:00:00 * DATE/TIME END: 2008-03-12T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.04 m * MAXIMUM DEPTH, sediment/rock: 4.37 m |
|---|---|
| Data(s) |
24/08/2012
|
| Formato |
text/tab-separated-values, 111 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.787758 doi:10.1594/PANGAEA.787758 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.787780 Opitz, Stephan; Wünnemann, Bernd; Aichner, Bernhard; Dietze, Elisabeth; Hartmann, Kai; Herzschuh, Ulrike; IJmker, Janneke; Lehmkuhl, Frank; Li, Shijie; Mischke, Steffen; Plotzki, Anna; Stauch, Georg; Diekmann, Bernhard (2012): Late Glacial and Holocene development of Lake Donggi Cona, north-eastern Tibetan Plateau, inferred from sedimentological analysis. Palaeogeography, Palaeoclimatology, Palaeoecology, 337-338, 159-176, doi:10.1016/j.palaeo.2012.04.013 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AWI_PerDyn; Beckman Coulter Laser diffraction particle size analyzer LS 200; China2008; COMPCORE; Composite Core; DEPTH, sediment/rock; Lake Donggi Cona, Qinghai, China; Periglacial Dynamics @ AWI; PG1904; Sampling/drilling in lake; Sand; Silt; Size fraction < 0.002 mm, > 9 phi, clay |
| Tipo |
Dataset |
