Geometry and morphology of buried channels (Typ I)


Autoria(s): Dittmers, Klaus Hauke; Niessen, Frank; Stein, Ruediger
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

Data(s)

15/12/2005

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