Geometry and morphology of the paleo-Ob River channels (Typ II)
| Cobertura |
MEDIAN LATITUDE: 75.344167 * MEDIAN LONGITUDE: 74.327917 * SOUTH-BOUND LATITUDE: 73.240000 * WEST-BOUND LONGITUDE: 66.420000 * NORTH-BOUND LATITUDE: 76.930000 * EAST-BOUND LONGITUDE: 76.920000 |
|---|---|
| Data(s) |
15/12/2005
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| Formato |
text/tab-separated-values, 144 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.338934 doi:10.1594/PANGAEA.338934 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.738340 Dittmers, Klaus Hauke (2006): Late Weichselian to Holocene sedimentation in the inner Kara Sea: Qualification and Quantification of Processes. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 523, 185 pp, doi:10.2312/BzPM_0523_2006 Dittmers, Klaus Hauke; Niessen, Frank; Stein, Ruediger (2008): Late Weichselian Fluvial Evolution on the Southern Kara Sea Shelf, North Siberia. Global and Planetary Change, 60(3-4), 327-350, doi:10.1016/j.gloplacha.2006.12.006 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AWI_Paleo; Bankful depth; Bankful width; Bankful width/depth ratio; Calculated; Depression; Depth, bathymetric; LATITUDE; LONGITUDE; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; ParaSound (Atlas Hydrographic); Sediment thickness; Siberian River Run-Off; SIRRO |
| Tipo |
Dataset |
