Geometry and morphology of buried channels (Typ I)
Cobertura |
MEDIAN LATITUDE: 74.610000 * MEDIAN LONGITUDE: 78.245000 * SOUTH-BOUND LATITUDE: 72.970000 * WEST-BOUND LONGITUDE: 72.420000 * NORTH-BOUND LATITUDE: 76.600000 * EAST-BOUND LONGITUDE: 88.850000 |
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Data(s) |
15/12/2005
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Formato |
text/tab-separated-values, 288 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.338932 doi:10.1594/PANGAEA.338932 |
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; Narrow Beam Sounder; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Sediment thickness; Siberian River Run-Off; SIRRO |
Tipo |
Dataset |