Late Quaternary lithofacies, provenance, and depositional environments (∼12–30 cal ka), north and south of the Denmark Strait
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology,Oceanography
Reference86 articles.
1. Andrews, J.T., Helgadottir, G., 2003. Late Quaternary ice cap extent and deglaciation of Hunafloaall, NorthWest Iceland: Evidence from marine cores. Arctic, Antarctic, and Alpine Research 35, in press.
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3. The measurement of sediment color using the colortron spectrophotometer;Andrews;Arct. Alp. Res.,1996
4. Spatial and temporal patterns of iceberg rafting (IRD) along the East Greenland margin ca. 68 N, over the last 14 cal. ka;Andrews;J. Quat. Sci.,1997
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2. Denmark Strait during the Late Glacial Maximum and Marine Isotope Stage 3: Sediment sources and transport processes;Marine Geology;2017-08
3. Holocene ice-rafting and sediment transport from the glaciated margin of East Greenland (67–70°N) to the N Iceland shelves: detecting and modelling changing sediment sources;Quaternary Science Reviews;2014-05
4. Multidecadal to millennial marine climate oscillations across the Denmark Strait (~ 66° N) over the last 2000 cal yr BP;Climate of the Past;2014-02-14
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