Source and climatic implication of the reactive iron and reactive silicate concentration found in a core from Meserve Glacier, Antartica
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v009/i003/GL009i003p00190/GL009i003p00190.pdf
Reference18 articles.
1. Dry valleys, Antarctica 1973-1974;Anderson;N.Z. Hydrol. Res. Ann. Rpt.,1976
2. Reduction of contamination problems in sampling of Antarctic snows for trace element analysis;Boutron;Anal. Chem. Acta,1979
3. Trace element content in East Antarctic snows since 1914;Boutron;Nature,1979
4. Sources of twelve trace metals in Antarctic snows determined by principal component analysis;Boutron;Jour. Geophys. Res.,1980
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