Calcium intensity of sediment core PG1784


Autoria(s): 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
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: 0.03 m * MAXIMUM DEPTH, sediment/rock: 1.70 m

Data(s)

24/08/2012

Formato

text/tab-separated-values, 168 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.787769

doi:10.1594/PANGAEA.787769

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; Calcium; China2006; DEPTH, sediment/rock; Gravity corer (Russian type); Lake Donggi Cona, Qinghai, China; Periglacial Dynamics @ AWI; PG1784; RGC; Sampling/drilling in lake; X-ray fluorescence core scanner (XRF), AWI
Tipo

Dataset