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The role of grounding-line sediment supply in ice-sheet advances and growth on continental shelves

An example from the mid-Norwegian sector of the Fennoscandian ice sheet during the Saalian and Weichselian

Bibliographic Data

ID14976100
AuthorsK I Torbjørn Dahlgren, Tore O Vorren, Jan Sverre Laberg (0000-0003-3917-4895)
Year2002
Volume95-96
Pages25-33
Publication date2002-09-01
Open AccessYes
TypeARTICLE
VenueQuaternary International (JOURNAL)
Journal identifiersISSN: 1040-6182 • E-ISSN: 1873-4553
PublisherElsevier BV (PUBLISHER)
DOI10.1016/s1040-6182(02)00024-1
OpenAlexW2065868998
LanguageEN
References cited29

Continental Margin · Continental shelf · Contourite · Cryosphere · Debris · Deposition (geology · Geomorphology · Glacial period · Glacier · Ice sheet · Ice shelf · Ice stream · Ice tongue · Iceberg · Pleistocene · Sea ice · Sediment · Sedimentary depositional environment · Tectonics · Turbidite · Cryospheric studies and observations · Geological formations and processes · Geology and Paleoclimatology Research · Geology · Oceanography · Paleontology

Highly citedNo

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Open DOISci-Hub
Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae