Measurements of cosmic-ray-produced 14 C in firn and ice from antarctica

We have studied the levels of 14 C in firn and ice from two regions accumulating ice in Antarctica, Dome C, and Newall Glacier. The observed concentrations indicate variable amounts of in-situ 14 C from cosmic-ray spallation of oxygen. 14 C appears to be produced as both CO and CO 2 in variable amou...

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Bibliographic Details
Main Authors: Timothy Jull, A. J., Lal, Devendra, Donahue, Douglas J., Mayewski, P., Lorius, C., Raynaud, D., Petit, J. R.
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier Science 1994
Subjects:
Online Access:http://repository.ias.ac.in/19249/
http://linkinghub.elsevier.com/retrieve/pii/0168583X94960283