Magnetic susceptibility, organic carbon, total sulphur and U-ratio as grainsize index on the Schwalbenberg II loess-paleosol sequence
| Cobertura |
LATITUDE: 50.557000 * LONGITUDE: 7.236000 * MINIMUM SECTION, height: 0.038 m * MAXIMUM SECTION, height: 12.940 m |
|---|---|
| Data(s) |
04/12/2015
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| Formato |
text/tab-separated-values, 2160 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.855567 doi:10.1594/PANGAEA.855567 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.855547 Profe, Jörn; Zolitschka, Bernd; Schirmer, Wolfgang; Frechen, Manfred; Ohlendorf, Christian (2016): Geochemistry unravels MIS 3/2 paleoenvironmental dynamics at the loess-paleosol sequence Schwalbenberg II, Germany. Palaeogeography, Palaeoclimatology, Palaeoecology, 459, 537-551, doi:10.1016/j.palaeo.2016.07.022 Schirmer, Wolfgang (2012): Rhine loess at Schwalbenberg II - MIS 4 and 3. E&G - Eiszeitalter und Gegenwart - Quaternary Science Journal, 61(1)32-47, doi:10.3285/eg.61.1.03 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #after Dearing et al. (1996); Bartington MS2B bulk 4650 Hz, Bremen; Bartington MS2B bulk 465 Hz, Bremen; Carbon, organic, total; Combustion at 480°C in a Dimatec laboratory furnace (Schirmer, 2012); Grain Size, gravity; Lithology/composition/facies; Magnetic susceptibility, frequency dependence; Magnetic susceptibility, frequency dependence, standard deviation; Outcrop; OUTCROP; Sample ID; Schwalbenberg_II; SECTION, height; Susceptibility, specific, high-field mass-normalized; Susceptibility, specific, high-field mass-normalized, standrad deviation; Susceptibility, specific, low-field mass-normalized; Susceptibility, specific, low-field mass-normalized, standard deviation; U-ratio |
| Tipo |
Dataset |
