Magnetic susceptibility of sediment core PS2551-1 from the Bellingshausen Sea, Antarctic
Cobertura |
LATITUDE: -69.815000 * LONGITUDE: -117.025000 * DATE/TIME START: 1994-03-03T17:38:00 * DATE/TIME END: 1994-03-03T17:38:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 10.83 m |
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Data(s) |
06/12/2007
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Formato |
text/tab-separated-values, 1084 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.671631 doi:10.1594/PANGAEA.671631 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
Hillenbrand, Claus-Dieter (2000): Glazialmarine Sedimentationsentwicklung am westantarktischen Kontinentalrand im Amundsen- und Bellingshausenmeer - Hinweise auf Paläoumweltveränderungen während der quartären Klimazyklen (Glaciomarine sedimentation on the continental margins of the Amundsen and Bellingshausen Seas, West Antarctica - indications for paleoenvironmental changes during the Quaternary climatic cycles). Berichte zur Polarforschung = Reports on Polar Research, 346, 182 pp, doi:10.2312/BzP_0346_2000 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #Amundsen Sea; ANT-XI/3; AWI_Paleo; DEPTH, sediment/rock; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2551-1; PS29; PS29/067; SL; Susceptibility, volume |
Tipo |
Dataset |