Mineral composition of sediment core PG1784
| Cobertura |
LATITUDE: 35.253910 * LONGITUDE: 98.508680 * DATE/TIME START: 2006-08-28T00:00:00 * DATE/TIME END: 2006-08-28T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.030 m * MAXIMUM DEPTH, sediment/rock: 1.670 m |
|---|---|
| Data(s) |
24/08/2012
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| Formato |
text/tab-separated-values, 86 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.787759 doi:10.1594/PANGAEA.787759 |
| 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 | #Aragonite, Intensity; AWI_PerDyn; Calcite, intensity; China2006; DEPTH, sediment/rock; Gravity corer (Russian type); Lake Donggi Cona, Qinghai, China; Periglacial Dynamics @ AWI; PG1784; Quartz, intensity; RGC; Sampling/drilling in lake; X-ray diffractometry (Philips PW1820) |
| Tipo |
Dataset |
