(Table 1) Rock magnetic parameters of core samples obtained from Morne Rouge, Ile de Possession
Cobertura |
LATITUDE: -46.391460 * LONGITUDE: 51.812970 * MINIMUM DEPTH, sediment/rock: 0.32 m * MAXIMUM DEPTH, sediment/rock: 4.12 m |
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Data(s) |
26/07/2008
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Resumo |
The magnetic high field susceptibility chi(hifi) indicates the presence of mafic paramagnetic minerals in the scoriae and points to an absence of clay minerals, and in turn of pedogenic processes, in the peat samples. Due to their volcanic origin, scoriae contain much more ferrimagnetic minerals than peat with is indicated by their enhanced saturation remanence Mrs. |
Formato |
text/tab-separated-values, 44 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.786585 doi:10.1594/PANGAEA.786585 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.786588 Van der Putten, Nathalie; Hébrard, Jean-Pierre; Verbruggen, Cyriel; Van de Vijver, Bart; Disnar, J R; Spassov, S; de Beaulieu, Jacques-Louis; De Dapper, M; Keravis, D; Hus, J; Thouveny, Nicolas; Frenot, Yves (2008): An integrated palaeoenvironmental investigation of a 6200 year old peat sequence from Ile de la Possession, Iles Crozet, sub-Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 270(1-2), 179-195, doi:10.1016/j.palaeo.2008.09.014 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #Bartington MS2 magnetic susceptibility meter; DEPTH, sediment/rock; Hand push corer; HSR; Hysteresis, saturation remanence; Ile de la Possession, Crozet Islands, South Indian Ocean; Morne_Rouge; Sample ID; Sample type; Susceptibility, specific |
Tipo |
Dataset |