Clay mineral evidence of nepheloid layer contributions to the Heinrich layers in the northwest Atlantic
Authors:
- 1 February 1999
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 146 (1-4) , 211-228
Abstract
No abstract availableKeywords
This publication has 39 references indexed in Scilit:
- An ice shelf mechanism for Heinrich layer productionPaleoceanography and Paleoclimatology, 1997
- Clay mineral signature of the NW Atlantic Boundary UndercurrentMarine Geology, 1996
- Shelf erosion and glacial ice proximity in the Labrador Sea during and after Heinrich events (H-3 or 4 to H-0) as shown by foraminiferaGeological Society, London, Special Publications, 1996
- Abrupt changes in marine conditions, Sunneshine Fiord, eastern Baffin Island, NWT during the last deglacial transition: Younger Dryas and H-0 eventsGeological Society, London, Special Publications, 1996
- Binge/purge oscillations of the Laurentide Ice Sheet as a cause of the North Atlantic's Heinrich eventsPaleoceanography and Paleoclimatology, 1993
- Patterns of Ice‐Rafted Detritus in the Glacial North Atlantic (40–55°N)Paleoceanography and Paleoclimatology, 1993
- Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 YearsQuaternary Research, 1988
- Age Dating and the Orbital Theory of the Ice Ages: Development of a High-Resolution 0 to 300,000-Year ChronostratigraphyQuaternary Research, 1987
- The Holocene sedimentary regime in the northern Mid-Atlantic Ridge regionEarth and Planetary Science Letters, 1986
- Mineralogical composition of the clay fraction of two fluvio-glacial sediments from east GreenlandClay Minerals, 1980