Luminescence dating of Late Quaternary sediments from East Greenland

Research output: Contribution to journal › Journal article › Research › peer-review

Standard

Luminescence dating of Late Quaternary sediments from East Greenland. / Mejdahl, V.; Funder, Svend Visby.

In: Boreas, Vol. 23, 1994, p. 525-535.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Mejdahl, V & Funder, SV 1994, 'Luminescence dating of Late Quaternary sediments from East Greenland', Boreas, vol. 23, pp. 525-535.

APA

Mejdahl, V., & Funder, S. V. (1994). Luminescence dating of Late Quaternary sediments from East Greenland. Boreas, 23, 525-535.

Vancouver

Mejdahl V, Funder SV. Luminescence dating of Late Quaternary sediments from East Greenland. Boreas. 1994;23:525-535.

Author

Mejdahl, V. ; Funder, Svend Visby. / Luminescence dating of Late Quaternary sediments from East Greenland. In: Boreas. 1994 ; Vol. 23. pp. 525-535.

Bibtex

@article{13def1df4bed48c4bedfdfbe98ff76fe,
title = "Luminescence dating of Late Quaternary sediments from East Greenland",
abstract = "Luminescence dating based on K-feldspars and using both TL and OSL methods have been performed on 94 sediment samples from East Greenland. The ages go back more than 380 ka, but are mainly from the last interglaciation and the subsequent period and include both shallow-marine/coastal-fluvial and ice proximal meltwater sediments. Independent age control indicates that the dates in the first group generally fall within ± 15% of the expected age, although a few samples show larger deviations. The ice proximal sediments, on the other hand, show a much larger spread and exaggerated ages, probably owing to incomplete bleaching. OSL may give better results than TL in these sediments",
author = "V. Mejdahl and Funder, {Svend Visby}",
year = "1994",
language = "English",
volume = "23",
pages = "525--535",
journal = "Boreas",
issn = "0300-9483",
publisher = "Wiley-Blackwell",

}

RIS

TY - JOUR

T1 - Luminescence dating of Late Quaternary sediments from East Greenland

AU - Mejdahl, V.

AU - Funder, Svend Visby

PY - 1994

Y1 - 1994

N2 - Luminescence dating based on K-feldspars and using both TL and OSL methods have been performed on 94 sediment samples from East Greenland. The ages go back more than 380 ka, but are mainly from the last interglaciation and the subsequent period and include both shallow-marine/coastal-fluvial and ice proximal meltwater sediments. Independent age control indicates that the dates in the first group generally fall within ± 15% of the expected age, although a few samples show larger deviations. The ice proximal sediments, on the other hand, show a much larger spread and exaggerated ages, probably owing to incomplete bleaching. OSL may give better results than TL in these sediments

AB - Luminescence dating based on K-feldspars and using both TL and OSL methods have been performed on 94 sediment samples from East Greenland. The ages go back more than 380 ka, but are mainly from the last interglaciation and the subsequent period and include both shallow-marine/coastal-fluvial and ice proximal meltwater sediments. Independent age control indicates that the dates in the first group generally fall within ± 15% of the expected age, although a few samples show larger deviations. The ice proximal sediments, on the other hand, show a much larger spread and exaggerated ages, probably owing to incomplete bleaching. OSL may give better results than TL in these sediments

M3 - Journal article

VL - 23

SP - 525

EP - 535

JO - Boreas

JF - Boreas

SN - 0300-9483

ER -

ID: 35221558