Susceptibility of sediment core HZM-4a
| Cobertura |
LATITUDE: 50.121230 * LONGITUDE: 6.877330 * DATE/TIME START: 1996-05-01T00:00:00 * DATE/TIME END: 1996-05-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 3.0000 m * MAXIMUM DEPTH, sediment/rock: 6.1990 m |
|---|---|
| Data(s) |
07/03/2000
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| Formato |
text/tab-separated-values, 8100 data points |
| Identificador | |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Zolitschka, Bernd (1998): Paläoklimatische Bedeutung laminierter Sedimente - Holzmaar (Eifel, Deutschland), Lake C2 (Nordwest-Territorien, Kanada) und Lago Grande di Monticchio (Basilikata, Italien). Relief Boden Paläoklima, Gebr. Bornträger, Berlin, Stuttgart, 13, 176 pp |
| Direitos |
Access constraints: access rights needed |
| Palavras-Chave | #Bartington MS2C coil sensor; Changes in the Geo-Biosphere during the last 15000 years; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GeoBio15k; HZM-4a; PC; Piston corer; Susceptibility, volume |
| Tipo |
Dataset |
