Source and climatic implication of the reactive iron and reactive silicate concentration found in a core from Meserve Glacier, Antartica
Glaciochemistry has recently provided a useful tool in the study of snow accumulation rates (Herron and Langway, 1979; Bulter et al., 1980 Warburton and Young, 1981; Mayewski et al., in press) and the elucidation of long-term climatic change (Delmas et al., 1980; Thompson and Mosley-Thompson, 1981)...
Published in: | Geophysical Research Letters |
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Main Authors: | , |
Format: | Text |
Language: | unknown |
Published: |
DigitalCommons@UMaine
1982
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Subjects: | |
Online Access: | https://digitalcommons.library.umaine.edu/ers_facpub/186 https://doi.org/10.1029/GL009i003p00190 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1186/viewcontent/sourceclimaticimplication.pdf |