Fig. 7.1 Susceptibility of sediment core Lz1120
Cobertura |
LATITUDE: 40.938000 * LONGITUDE: 20.759000 * DATE/TIME START: 2005-03-16T00:00:00 * DATE/TIME END: 2005-03-16T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 11.96 m |
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Data(s) |
21/05/2011
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Formato |
text/tab-separated-values, 588 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.760956 doi:10.1594/PANGAEA.760956 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.760961 Wagner, Bernd; Reicherter, Klaus; Daut, Gerhard; Wessels, Martin; Matzinger, Andreas; Schwalb, Antje; Spirkovski, Zoran; Sanxhaku, Mitat (2008): The potential of Lake Ohrid for long-term palaeoenvironmental reconstructions. Palaeogeography, Palaeoclimatology, Palaeoecology, 259, 341-356, doi:10.1016/j.palaeo.2007.10.015 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #DEPTH, sediment/rock; Lake Ohrid, Macedonian/Albanian border; Lz1120; Multi-Sensor Core Logger, GEOTEK; ohrid-exp; PCUWI; Piston corer (Uwitec); Sampling/drilling in lake; Susceptibility, volume |
Tipo |
Dataset |