Mots-clés
Bloc erratique ; British Columbia ; Calotte glaciaire ; Canada ; Datation ; Datation C 14 ; Datation isotopique ; Déglaciation ; Etats-Unis ; Lithologie ; Moraine ; Paléo-environnement ; Pléistocène ; Quaternaire ; Washington StateBritish Columbia ; C 14 dating ; Canada ; Dating ; Deglaciation ; Erratic boulder ; Ice sheet ; Isotope dating ; Lithology ; Moraine ; Palaeo-environment ; Pleistocene ; Quaternary ; United States of America ; Washington StateDetermination of Cl 36 production rates derived from the well-dated deglaciation surfaces of Whidbey and Fidalgo Islands, Washington
Auteurs :SWANSON, T.W.
CAFFEE, M.
Description :
This experimental work includes both the actual determination of production rates and their subsequent validation. The production rates were determined using 50 calibration samples collected from northern Puget lowland. The validation set consists of 23 samples collected from a late Pleistocene dacite flow in southwestern British Columbia and three disparate deglaciated localities in northern Washington and southern British Columbia. The dacite flow and the three deglaciation localities are dated by limiting C 14 ages.
Type de document :
Article de périodique
Source :
Quaternary research, issn : 0033-5894, 2001, vol. 56, n°. 3, p. 366-382, nombre de pages : 17, Collation : Illustration, Références bibliographiques : 56 ref.
Date :
2001
Editeur :
Pays édition : Etats-Unis, San Diego, CA, Elsevier
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)