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Weathering of surface clasts as an indicator of the relative age of glacial deposits on Jameson Land, East Greenland
Ansvarlig organisasjon
1994 (engelsk)Inngår i: Boreas, Vol. 23, nr 4, s. 473-478Artikkel i tidsskrift (Fagfellevurdert)
Abstract [en]
The relative age of glacial deposits on Jameson Land was investigated by weathering-based techniques. Two related methods, measurement of rind thickness and of Schmidt hammer rebound values. were added to a dating programme of luminescence-, amino acid- and 14C-analyses. Rind thicknesses differ significantly between areas which represent three glacial phascs, spanning a time interval from late Saale to Late Weichselian. Rebound values are more susceptible to external factors than the rind values but may, if these external factors are known, serve as a complement to the interpretation of rind development.
sted, utgiver, år, opplag, sider
1994, 16 JAN 2008. Vol. 23, nr 4, s. 473-478
Emneord [en]
PONAM, SWEDARCTIC 1992, SWEDARCTIC 1990, Quaternary geology, Arctic, Greenland, East Greenland, Jameson Land, glacial deposits
Identifikatorer
URN: urn:nbn:se:polar:diva-1100DOI: 10.1111/j.1502-3885.1994.tb00614.xOAI: oai:DiVA.org:polar-1100DiVA, id: diva2:569236
Merknad

Source: Polardok by Swedish Polar Research Secretariat

Tilgjengelig fra: 2012-11-15 Laget: 2012-11-15 Sist oppdatert: 2012-11-15

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